Takes of Marine Mammals Incidental to Specified Activities; Low-Energy Marine Geophysical Survey in the Dumont d'Urville Sea Off the Coast of East Antarctica, January to March 2013, 463-497 [2013-31471]
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National Oceanic and Atmospheric Administration
Takes of Marine Mammals Incidental to Specified Activities; Low-Energy
Marine Geophysical Survey in the Dumont d’Urville Sea Off the Coast of
East Antarctica, January to March 2013; Notice
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric
Administration
RIN 0648–XC779
Takes of Marine Mammals Incidental to
Specified Activities; Low-Energy
Marine Geophysical Survey in the
Dumont d’Urville Sea Off the Coast of
East Antarctica, January to March 2013
National Marine Fisheries
Service (NMFS), National Oceanic and
Atmospheric Administration (NOAA),
Commerce.
ACTION: Notice; proposed Incidental
Harassment Authorization; request for
comments.
AGENCY:
NMFS has received an
application from the National Science
Foundation (NSF) Division of Polar
Programs, and Antarctic Support
Contract (ASC) on behalf of five
research institutions: Colgate
University, Columbia University, Texas
A&M Research Foundation, University
of South Florida, and University of
Texas at Austin, for an Incidental
Harassment Authorization (IHA) to take
marine mammals, by harassment,
incidental to conducting a low-energy
marine geophysical (seismic) survey in
the Dumont d’Urville Sea off the coast
of East Antarctica, January to March
2014. Pursuant to the Marine Mammal
Protection Act (MMPA), NMFS is
requesting comments on its proposal to
issue an IHA to NSF to incidentally
harass, by Level B harassment only, 14
species of marine mammals during the
specified activity.
DATES: Comments and information must
be received no later than February 3,
2014.
SUMMARY:
Comments on the
application should be addressed to
P. Michael Payne, Chief, Permits and
Conservation Division, Office of
Protected Resources, National Marine
Fisheries Service, 1315 East-West
Highway, Silver Spring, MD 20910. The
mailbox address for providing email
comments is ITP.Goldstein@noaa.gov.
NMFS is not responsible for email
comments sent to addresses other than
the one provided here. Comments sent
via email, including all attachments,
must not exceed a 10-megabyte file size.
All comments received are a part of
the public record and will generally be
posted to https://www.nmfs.noaa.gov/pr/
permits/incidental.htm#applications
without change. All Personal Identifying
Information (for example, name,
address, etc.) voluntarily submitted by
the commenter may be publicly
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ADDRESSES:
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accessible. Do not submit confidential
business information or otherwise
sensitive or protected information.
A copy of the application containing
a list of the references used in this
document may be obtained by writing to
the above address, telephoning the
contact listed here (see FOR FURTHER
INFORMATION CONTACT) or visiting the
internet at: https://www.nmfs.noaa.gov/
pr/permits/incidental.htm#applications.
NSF and ASC have provided a ‘‘Draft
Initial Environmental Evaluation/
Environmental Assessment to Conduct a
Marine-Based Studies of the Totten
Glacier System and Marine Record of
Cryosphere—Ocean Dynamics’’ (IEE/
EA), prepared by AECOM, on behalf of
NSF and ASC, which is also available at
the same Internet address. Documents
cited in this notice may be viewed, by
appointment, during regular business
hours, at the aforementioned address.
FOR FURTHER INFORMATION CONTACT:
Howard Goldstein or Jolie Harrison,
Office of Protected Resources, NMFS,
301–427–8401.
SUPPLEMENTARY INFORMATION:
Background
Section 101(a)(5)(D) of the MMPA, as
amended (16 U.S.C. 1371 (a)(5)(D)),
directs the Secretary of Commerce
(Secretary) to authorize, upon request,
the incidental, but not intentional,
taking of small numbers of marine
mammals of a species or population
stock, by United States citizens who
engage in a specified activity (other than
commercial fishing) within a specified
geographical region if certain findings
are made and, if the taking is limited to
harassment, a notice of a proposed
authorization is provided to the public
for review.
Authorization for the incidental
taking of small numbers of marine
mammals shall be granted if NMFS
finds that the taking will have a
negligible impact on the species or
stock(s), and will not have an
unmitigable adverse impact on the
availability of the species or stock(s) for
subsistence uses (where relevant). The
authorization must set forth the
permissible methods of taking, other
means of effecting the least practicable
adverse impact on the species or stock
and its habitat, and requirements
pertaining to the mitigation, monitoring
and reporting of such takings. NMFS
has defined ‘‘negligible impact’’ in 50
CFR 216.103 as ‘‘. . . an impact
resulting from the specified activity that
cannot be reasonably expected to, and is
not reasonably likely to, adversely affect
the species or stock through effects on
annual rates of recruitment or survival.’’
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Section 101(a)(5)(D) of the MMPA
established an expedited process by
which citizens of the United States can
apply for an authorization to
incidentally take small numbers of
marine mammals by harassment.
Section 101(a)(5)(D) of the MMPA
establishes a 45-day time limit for
NMFS’s review of an application
followed by a 30-day public notice and
comment period on any proposed
authorizations for the incidental
harassment of small numbers of marine
mammals. Within 45 days of the close
of the public comment period, NMFS
must either issue or deny the
authorization.
Except with respect to certain
activities not pertinent here, the MMPA
defines ‘‘harassment’’ as: Any act of
pursuit, torment, or annoyance which (i)
has the potential to injure a marine
mammal or marine mammal stock in the
wild [Level A harassment]; or (ii) has
the potential to disturb a marine
mammal or marine mammal stock in the
wild by causing disruption of behavioral
patterns, including, but not limited to,
migration, breathing, nursing, breeding,
feeding, or sheltering [Level B
harassment].
Summary of Request
On July 3, 2013, NMFS received an
application from the NSF and ASC
requesting that NMFS issue an IHA for
the take, by Level B harassment only, of
small numbers of marine mammals
incidental to conducting a low-energy
marine seismic survey in International
Waters (i.e., high seas) and in the
Southern Ocean off the coast of East
Antarctica during January to March
2014. We received an addendum to the
application from the NSF and ASC on
December 18, 2013 which reflected
updates to incidental take requests for
marine mammals related to icebreaking
activities.
The research would be conducted by
five research institutions: Colgate
University, Columbia University, Texas
A&M Research Foundation, University
of South Florida, and University of
Texas at Austin. The NSF and ASC
plans to use one source vessel, the R/
VIB Nathaniel B. Palmer (Palmer), and
a seismic airgun array to collect seismic
data in the Southern Ocean. The vessel
would be operated by ASC, which
operates the United States Antarctic
Program under contract to the NSF. In
support of the United States Antarctic
Program, the NSF and ASC plans to use
conventional low-energy, seismic
methodology to perform marine-based
studies in the Dumont d’Urville Sea to
include evaluation of geophysical and
physical oceanographic features in two
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areas along the coast of East Antarctica
(see Figures 1, 2, and 3 of the IHA
application). The primary area proposed
for the study is the Totten Glacier
system (preferred study area) including
the Moscow University Ice Shelf along
the Sabrina Coast, and a secondary area,
the Mertz Glacier and Cook Ice Shelf,
along the Oates Coast. In addition to the
proposed operations of the seismic
airgun array and hydrophone streamer,
NSF and ASC intend to operate a singlebeam echosounder, multi-beam
echosounder, acoustic Doppler current
profiler (ADCP), and sub-bottom profiler
continuously throughout the survey.
Acoustic stimuli (i.e., increased
underwater sound) generated during the
operation of the seismic airgun array
and from icebreaking activities may
have the potential to cause a behavioral
disturbance for marine mammals in the
survey area. This is the principal means
of marine mammal taking associated
with these activities, and NSF and ASC
has requested an authorization to take
14 species of marine mammals by Level
B harassment. Take is not expected to
result from the use of the single-beam
echosounder, multi-beam echosounder,
ADCP, acoustic locator, and sub-bottom
profiler, as the brief exposure of marine
mammals to one pulse, or small
numbers of signals, in this particular
case is not likely to result in the
harassment of marine mammals. Also,
NMFS does not expect take to result
from collision with the source vessel
because it is a single vessel moving at
a relatively slow, constant cruise speed
of 5 knots [kts]; 9.3 kilometers per hour
[km/hr]; 5.8 miles per hour [mph])
during seismic acquisition within the
survey, for a relatively short period of
time (approximately 45 operational
days). It is likely that any marine
mammal would be able to avoid the
vessel.
Description of the Proposed Specified
Activity
NSF and ASC propose to conduct a
low-energy seismic survey in the
Dumont d’Urville Sea in the Southern
Ocean off the coast of East Antarctica
from January to March 2014. In addition
to the low-energy seismic survey,
scientific activities would include
conducting a bathymetric profile survey
of the seafloor using transducer based
instruments such as a multi-beam
echosounder and sub-bottom profiler;
conducting magnetometry and imaging
surveys using an underwater camera
assembly; collecting sediment cores and
dredge sampling; and collecting water
samples and conductivity (salinity),
temperature, depth (CTD) and current
data through the deployment and
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recovery of short-term (in place for
approximately one month) and longterm (in place for approximately one
year) instrumentation moorings, CTD
equipment casts, and the use of
transducer-based ADCP instruments.
Sea ice conditions will dictate areas
where the ship and airguns can operate.
Due to dynamic ice conditions, which
cannot be predicted on a local scale, it
is not possible to develop tracklines a
priori. The seismic survey would be
conducted in one or both of the two
study areas depending on the sea ice
conditions; however, the preferred
study area is the Totten Glacier region
(see Figure 2 of the IHA application).
Water depths in the survey area range
from 100 to 1,000 meters (m) (328.1 to
3,280.1 feet [ft]), and possibly exceeding
1,000 m in some areas. The seismic
surveys are scheduled to occur for a
total of less than or equal to 300 hours
at one or both of the two study areas for
approximately 45 operational days in
January to March 2014. The operation
hours and survey length would include
equipment testing, ramp-up, line
changes, and repeat coverage. The long
transit time between port and the study
site constrains how long the ship can be
in the study area and effectively limits
the maximum amount of time the
airguns can operate. Some minor
deviation from these dates would be
possible, depending on logistics and
weather.
The proposed survey of Totten Glacier
and Moscow University Ice Shelf along
the Sabrina Coast continental shelf is
designed to address several critical
questions. The Totten Glacier system,
which drains one-eighth of the East
Antarctic Ice Sheet and contains more
ice volume than the entire West
Antarctic Ice Sheet, remains the single
largest and least understood glacial
system which possesses a potentially
unsteady dynamic. If it were to melt,
sea-level would rise by more than 5 m
(16.4 ft) worldwide. The proposed
marine studies would help to
understand both the dynamics and the
controls of the Totten Glacier system,
and to resolve ambiguity in large ice
mass dynamic behavior. This research
would be accomplished via the
collection of glaciological, geological,
and physical oceanographic data. In
order to place the modern system, as
well as more recent changes to the
system, into a longer-term perspective,
researchers would collect and interpret
marine geologic, geochemical, and
geophysical records of the longer term
behavior and response of this system.
The proposed research would
complement fieldwork studying other
Antarctic ice shelves oceanographic
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studies near the Antarctic Peninsula,
and ongoing development of ice sheet
and other ocean models. It would
facilitate learning at sea and ashore by
students, help to fill important spatial
and temporal gaps in a sparsely sampled
region of coastal Antarctica, and
communicate its findings via
publications and outreach. Obtaining
records of currents and oceanographic
properties in this region are consistent
with the objectives of the Southern
Ocean Observing System for climate
change. The work would enhance
general understanding of air-sea-ice
interactions, ocean circulation, ice shelf
sensitivity to climate change, and the
present and future roles of East
Antarctic Ice Sheet on sea level.
The Principal Investigators are Dr.
Amy Leventer of Colgate University, Dr.
Donald Blankenship and Dr. Sean
Gulick of the University of Texas at
Austin, Dr. Eugene Domack of the
University of South Florida, Mr. Bruce
Huber of Columbia University, and Dr.
Alejandro Orsi of Texas A&M Research
Foundation.
The procedures to be used for the
surveys would be similar to those used
during previous low-energy seismic
surveys by NSF and would use
conventional seismic methodology. The
proposed survey will involve one source
vessel, the R/V Nathaniel B. Palmer
(Palmer). NSF and ASC will deploy two
(each with a discharge volume of 45
cubic inch [in3] with a total volume of
90 in3 or each with a discharge volume
of 105 in3 with a total volume of 210
in3) Sercel Generator Injector (GI) airgun
array as an energy source at a tow depth
of up to 3 m (9.8 ft) below the surface
(more information on the airguns can be
found in Appendix B of the IHA
application). The receiving system will
consist of one 100 m (328.1 ft) long, 24channel, solid-state hydrophone
streamer towed behind the vessel. As
the GI airguns are towed along the
survey lines, the hydrophone streamer
will receive the returning acoustic
signals and transfer the data to the
onboard processing system. All planned
seismic data acquisition activities will
be conducted by technicians provided
by NSF and ASC with onboard
assistance by the scientists who have
proposed the study. The vessel will be
self-contained, and the crew will live
aboard the vessel for the entire cruise.
The planned seismic survey (e.g.,
equipment testing, start-up, line
changes, repeat coverage of any areas,
and equipment recovery) will consist of
approximately 2,800 kilometer (km)
(1,511.9 nautical miles [nmi]) of transect
lines (including turns) in the survey
area in the Dumont d’Urville Sea of the
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Southern Ocean (see Figures 1, 2, and 3
of the IHA application). In addition to
the operation of the airgun array, a
single-beam and multi-beam
echosounder, ADCP, and a sub-bottom
profiler will also likely be operated from
the Palmer continuously throughout the
cruise between the first and last survey
sites. There will be additional seismic
operations associated with equipment
testing, ramp-up, and possible line
changes or repeat coverage of any areas
where initial data quality is substandard. In NSF and ASC’s estimated
take calculations, 25% has been added
for those additional operations.
TABLE 1—PROPOSED LOW-ENERGY SEISMIC SURVEY ACTIVITIES IN THE DUMONT D’URVILLE SEA OFF THE COAST OF
EAST ANTARCTICA
Survey length
(km)
Cumulative
duration
(hr) 1
2,800 (1,511.9 nmi) ................
≤300
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1 Airgun
Airgun array total volume
2 × 45 in3 (2 × 737 cm3) or
2 × 105 in3 (2 × 1,720 cm3)
Time between airgun shots
(distance)
5 seconds (12.5 m or 41 ft) ...
Streamer length
(m)
100 (328.1 ft).
operations are planned for no more than 16 continuous hours at a time.
Vessel Specifications
The Palmer, a research vessel owned
by Edison Chouest Offshore, Inc. and
operated by NSF and ACS (under a
long-term charter with Edison Chouest
Offshore, Inc.), will tow the two GI
airgun array, as well as the hydrophone
streamer. When the Palmer is towing the
airgun array and the relatively short
hydrophone streamer, the turning rate of
the vessel while the gear is deployed is
much higher than the limit of 5 degrees
per a minute for a seismic vessel towing
a streamer of more typical length (much
greater than 1 km [0.5 nmi]), which is
approximately 20 degrees. Thus, the
maneuverability of the vessel is not
limited much during operations with
the streamer.
The U.S.-flagged vessel has a length of
94 m (308.5 ft); a beam of 18.3 m (60 ft);
a maximum draft of 6.8 m (22.5 ft); and
a gross tonnage of 6,174. The ship is
powered by four Caterpillar 3608 diesel
engines (3,300 brake horsepower [hp] at
900 rotations per minute [rpm]) and a
1,400 hp flush-mounted, water jet
azimuthing bowthruster. Electrical
power is provided by four Catepillar
3512, 1,050 kiloWatt (kW) diesel
generators. The Palmer’s operation
speed during seismic acquisition is
typically approximately 9.3 km/hr (5
kts) (varying between 7.4 to 11.1 km/hr
[4 to 6 kts]). When not towing seismic
survey gear, the Palmer typically cruises
at 18.7 km/hr (10.1 kts) and has a
maximum speed of 26.9 km/hr (14.5
kts). The Palmer has an operating range
of approximately 27,780 km (15,000
nmi) (the distance the vessel can travel
without refueling), which is
approximately 70 to 75 days. The vessel
can accommodate 37 scientists and 22
crew members.
The vessel also has two locations as
likely observation stations from which
Protected Species Observers (PSO) will
watch for marine mammals before and
during the proposed airgun operations
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on the Palmer. Observing stations will
be at the bridge level with PSO’s eye
level approximately 16.5 m (54.1 ft)
above sea level with an approximately
270° view around the vessel, and an
aloft observation tower that is
approximately 24.4 m (80.1 ft) above sea
level that is protected from the weather
and has an approximately 360° view
around the vessel. More details of the
Palmer can be found in the IHA
application and online at: https://
www.nsf.gov/geo/plr/support/
nathpalm.jsp and https://www.usap.gov/
vesselScienceAndOperations/
contentHandler.cfm?id=1561.
Acoustic Source Specifications
Seismic Airguns
The Palmer will deploy an airgun
array, consisting of two 45 in3 or two
105 in3 GI airguns as the primary energy
source and a 100 m streamer containing
hydrophones. The airgun array will
have a supply firing pressure of 2,000
pounds per square inch (psi) and 2,200
psi when at high pressure stand-by (i.e.,
shut-down). The regulator is adjusted to
ensure that the maximum pressure to
the GI airguns is 2,000 psi, but there are
times when the GI airguns may be
operated at pressures as low as 1,750 to
1,800 psi Seismic pulses for the GI
airguns will be emitted at intervals of
approximately 5 seconds. At speeds of
approximately 9.3 km/hr, the shot
intervals correspond to spacing of
approximately will be 12.5 m (41 ft)
during the study. There would be
approximately 720 shots per hour.
During firing, a brief (approximately
0.03 second) pulse sound is emitted; the
airguns will be silent during the
intervening periods. The dominant
frequency components range from two
to 188 Hertz (Hz).
The GI airguns would be used in
harmonic mode, that is, the volume of
the injector chamber (I) of each GI
airgun is equal to that of its generator
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chamber (G): 45 in3 and 105 in3 for each
airgun array. Each airgun would be
initially configured to a displacement
volume of 45 in3 for the generator and
injector. The generator chamber of each
GI airgun in the primary source, the one
responsible for introducing the sound
pulse into the ocean, is 45 in3. The
injector chamber injects air into the
previously-generated bubble to maintain
its shape, and does not introduce more
sound into the water. The airguns
would fire the compressed air volume in
unison in a harmonic mode. In
harmonic mode, the injector volume is
designed to destructively interfere with
the reverberations of the generator
(source component). Firing the airguns
in harmonic mode maximizes resolution
in the data and minimizes any excess
noise in the water column or data
caused by the reverberations (or bubble
pulses). The two GI airguns will be
spaced approximately 3 or 6 m (9.8 or
19.7 ft) apart, side-by-side, between 15
and 40 m (49.2 and 131.2 ft) behind the
Palmer, at a depth of up to 3 m during
the surveys. If needed to improve
penetration of the strata, the two airguns
may be reconfigured to a displacement
volume of 105 in3 each and would still
be considered a low-energy acoustic
source as defined in the NSF/USGS
PEIS. Therefore, there are three possible
two airgun array configurations: Two
45/45 in3 airguns separated by 3 m, two
45/45 in3 airguns separated by 6 m, and
two 105/105 in3 airguns separated by 3
m. The two 45/45 in3 airguns separated
by 3 m layout is preferred, the two 45/
45 in3 separated by 6 m layout would
be used in the event the middle of the
three 45/45 in3 airgun fails, and the two
105/105 in3 airguns separated by 3 m
would be used only if additional
penetration is needed. To summarize,
two strings of GI airguns would be
available: (1) Three 45/45 in3 airguns on
a single string where one of these is
used as a ‘‘hot spare’’ in the event of
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failure of one of the other two airguns,
these three GI airguns are separated by
3 m; and (2) two 105/105 in3 airguns on
a second string without a ‘‘hot spare.’’
The total effective volume will be 90 or
210 in3. The two strings would be
spaced 14 m (45.9 ft) apart, on either
side of the midline of the vessel,
however, only one string at a time
would be used.
The Nucleus modeling software used
at Lamont-Doherty Earth Observatory of
Columbia University (L–DEO) does not
include GI airguns as part of its airgun
library, however signatures and
mitigation models have been obtained
for two 45 in3 G airguns at 2 m tow
depth and two 105 in3 G airguns at 3 m
tow depth that are close
approximations. For the two 45 in3
airgun array, the source output
(downward) is 230.6 dB re: 1 mPam for
0-to-peak and 235.9 dB re: 1 mPam for
peak-to-peak. For the two 105 in3 airgun
array, the source output (downward) is
234.4 dB re: 1 mPam 0-to-peak and 239.8
dB re: 1 mPam for peak-to-peak. These
numbers were determined using the
aforementioned G-airgun approximation
to the GI airgun and using signatures
filtered with DFS V out-256 Hz 72 dB/
octave. The dominant frequency range
would be 20 to 160 Hz for a pair of GI
airguns towed at 3 m depth and 35 to
230 Hz for a pair of GI airguns towed at
2 m depth.
During the low-energy seismic survey,
the vessel would attempt to maintain a
constant cruise speed of approximately
5 knots. The airguns would operate
continuously for no more than 16 hours
at a time and duration of continuous
operation is dependent on ice
concentration. The cumulative duration
of the airgun operations will not exceed
200 hrs. The relatively short, 24-channel
hydrophone streamer would provide
operational flexibility to allow the
seismic survey to proceed along the
designated cruise track with minimal
interruption due to variable sea ice
conditions. The design of the seismic
equipment is to achieve high-resolution
images of the glacial marine sequence
stratigraphy with the ability to correlate
to the ultra-high frequency sub-bottom
profiling data and provide crosssectional views to pair with the seafloor
bathymetry. The cruise path would be
designated once in the study area and
would take care to avoid heavy ice
conditions such as icebergs or dense
areas of pack ice that could potentially
damage the airguns or streamer and
minimize proximity to potential marine
receptors.
Weather conditions that could affect
the movement of sea ice and hinder the
hydrophone streamer would be closely
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monitored, as well as conditions that
could limit visibility. If situations are
encountered which pose a risk to the
equipment, impede data collection, or
require the vessel to stop forward
progress, the seismic survey equipment
would be shut-down and retrieved until
conditions improve. In general, the
hydrophone streamer and sources could
be retrieved in less than 30 minutes.
Metrics Used in This Document
This section includes a brief
explanation of the sound measurements
frequently used in the discussions of
acoustic effects in this document. Sound
pressure is the sound force per unit
area, and is usually measured in
micropascals (mPa), where 1 pascal (Pa)
is the pressure resulting from a force of
one newton exerted over an area of one
square meter. Sound pressure level
(SPL) is expressed as the ratio of a
measured sound pressure and a
reference level. The commonly used
reference pressure level in underwater
acoustics is 1 mPa, and the units for
SPLs are dB re: 1 mPa. SPL (in decibels
[dB]) = 20 log (pressure/reference
pressure).
SPL is an instantaneous measurement
and can be expressed as the peak, the
peak-to-peak (p-p), or the root mean
square (rms). Root mean square, which
is the square root of the arithmetic
average of the squared instantaneous
pressure values, is typically used in
discussions of the effects of sounds on
vertebrates and all references to SPL in
this document refer to the root mean
square unless otherwise noted. SPL does
not take the duration of a sound into
account.
Characteristics of the Airgun Pulses
Airguns function by venting highpressure air into the water which creates
an air bubble. The pressure signature of
an individual airgun consists of a sharp
rise and then fall in pressure, followed
by several positive and negative
pressure excursions caused by the
oscillation of the resulting air bubble.
The oscillation of the air bubble
transmits sounds downward through the
seafloor and the amount of sound
transmitted in the near horizontal
directions is reduced. However, the
airgun array also emits sounds that
travel horizontally toward non-target
areas.
The nominal downward-directed
source levels of the airgun arrays used
by NSF and ASC on the Palmer do not
represent actual sound levels that can be
measured at any location in the water.
Rather, they represent the level that
would be found 1 m (3.3 ft) from a
hypothetical point source emitting the
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same total amount of sound as is
emitted by the combined GI airguns.
The actual received level at any location
in the water near the GI airguns will not
exceed the source level of the strongest
individual source. In this case, that will
be about 224.6 dB re 1 mPam peak, or
229.8 dB re 1 mPam peak-to-peak for the
two 45 in3 airgun array, and 228.2 dB
re 1 mPam peak or 233.5 dB re 1 mPam
peak-to-peak for the two 105 in3 airgun
array. However, the difference between
rms and peak or peak-to-peak values for
a given pulse depends on the frequency
content and duration of the pulse,
among other factors. Actual levels
experienced by any organism more than
1 m from either GI airgun will be
significantly lower.
Accordingly, Lamont-Doherty Earth
Observatory of Columbia University (L–
DEO) has predicted and modeled the
received sound levels in relation to
distance and direction from the two GI
airgun array. A detailed description of
L–DEO’s modeling for this survey’s
marine seismic source arrays for
protected species mitigation is provided
in the NSF/USGS PEIS. These are the
nominal source levels applicable to
downward propagation. The NSF/USGS
PEIS discusses the characteristics of the
airgun pulses. NMFS refers the
reviewers to those documents for
additional information.
Predicted Sound Levels for the Airguns
To determine exclusion zones for the
airgun array to be used in the
intermediate and deep water of the Gulf
of Mexico (GOM), received sound levels
have been modeled by L–DEO for a
number of airgun configurations,
including two 45 in3 and two 105 in3 G
airguns, in relation to distance and
direction from the airguns (see Figure 2
and 3 in Attachment B of the IHA
application). The model does not allow
for bottom interactions, and is most
directly applicable to deep water.
Because the model results are for G
airguns, which have more energy than
GI airguns of the same size, those
distances overestimate (by
approximately 10%) the distances for
the two 45 in3 GI airguns and two 105
in3 GI airguns, respectively. Although
the distances are overestimated, no
adjustments for this have been made to
the radii distances in Table 2 (below).
Based on the modeling, estimates of the
maximum distances from the GI airguns
where sound levels of 190, 180, and 160
dB re 1 mPa (rms) are predicted to be
received in shallow, intermediate, and
deep water are shown in Table 2 (see
Table 1 of Attachment B of the IHA
application).
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Empirical data concerning the 190,
180, and 160 dB (rms) distances were
acquired for various airgun arrays based
on measurements during the acoustic
verification studies conducted by L–
DEO in the northern GOM in 2003
(Tolstoy et al., 2004) and 2007 to 2008
(Tolstoy et al., 2009; Diebold et al.,
2010). Results of the 18 and 36 airgun
array are not relevant for the two GI
airguns to be used in the proposed
survey. The empirical data for the 6, 10,
12, and 20 airgun arrays indicate that,
for deep water, the L–DEO model tends
to overestimate the received sound
levels at a given distance (Tolstoy et al.,
2004). Measurements were not made for
the two GI airgun array in deep water;
however, NSF and ASC proposes to use
the buffer and exclusion zones
predicted by L–DEO’s model for the
proposed GI airgun operations in deep
water, although they are likely
conservative given the empirical results
for the other arrays. Using the L–DEO
model, Table 2 (below) shows the
distances at which three rms sound
levels are expected to be received from
the two GI airguns. The 180 and 190 dB
re 1 mPam (rms) distances are the safety
criteria for potential Level A harassment
as specified by NMFS (2000) and are
applicable to cetaceans and pinnipeds,
respectively. If marine mammals are
detected within or about to enter the
appropriate exclusion zone, the airguns
will be shut-down immediately.
Tow depth
(m)
Source and total volume
Table 2 summarizes the predicted
distances at which sound levels (160,
180, and 190 dB [rms]) are expected to
be received from the two airgun array
(45 in3 or 105 in3) operating in shallow
(less than 100 m [328 ft]), intermediate
(100 to 1,000 m [328 to 3,280 ft]), and
deep water (greater than 1,000 m [3,280
ft]) depths.
Table 2— Predicted and modeled (two
45 in3 and two 105 in3 GI airgun array)
distances to which sound levels ≥190,
180 and 160 dB re: 1 mPa (rms) could
be received in shallow, intermediate,
and deep water during the proposed
low-energy seismic survey in the
Dumont d’Urville Sea of the Southern
Ocean, January to March 2014.
Predicted RMS radii distances
(m) for 2 GI airgun array
Water depth
(m)
160 dB
Two GI Airguns (45 in3) .............
3
Shallow (<100) ...................................
Two GI Airguns (45 in3) .............
3
Intermediate (100 to 1,000) ................
Two GI Airguns (45 in3) .............
3
Deep (≤1,000) ....................................
Two GI Airguns (105 in3) ...........
3
Shallow (<100) ...................................
Two GI Airguns (105 in3) ...........
3
Intermediate (100 to 1,000) ................
Two GI Airguns (105 in3) ...........
3
Deep (>1,000) ....................................
NMFS expects that acoustic stimuli
resulting from the proposed operation of
the two GI airgun array has the potential
to harass marine mammals. NMFS does
not expect that the movement of the
Palmer, during the conduct of the lowenergy seismic survey, has the potential
to harass marine mammals because of
the relatively slow operation speed of
the vessel (approximately 5 kts; 9.3 km/
hr; 5.8 mph) during seismic acquisition.
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Bathymetric Survey
Along with the low-energy airgun
operations, other additional geophysical
measurements would be made using
swath bathymetry, backscatter sonar
imagery, high-resolution sub-bottom
profiling (‘‘CHIRP’’), imaging, and
magnetometer instruments. In addition,
several other transducer-based
instruments onboard the vessel would
be operated continuously during the
cruise for operational and navigational
purposes. Operating characteristics for
the instruments to be used are described
below.
Single-Beam Echosounder (Knudsen
3260)—The hull-mounted CHIRP sonar
would be operated continuously during
all phases of the cruise. This instrument
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180 dB
1,176 ................
(3,858.3 ft) ........
600 ...................
(1,968.5 ft) ........
400 ...................
(1,312.3 ft) ........
1,970 ................
(6,463.3 ft) ........
1,005 ................
(3,297.2 ft) ........
670 ...................
(2,198.2 ft) ........
296 ...................
(971.1 ft) ...........
100 ...................
(328ft) ...............
100 ...................
(328 ft) ..............
511 ...................
(1,676.5 ft) ........
100 ...................
is operated at 12 kHz for bottomtracking purposes or at 3.5 kHz in the
sub-bottom profiling mode. The sonar
emits energy in a 30° beam from the
bottom of the ship.
Single-Beam Echosounder (Bathy
2000)—The hull-mounted sonar
characteristics of the Bathy 2000 are
similar to the Knudsen 3260. Only one
hull-mounted echosounder can be
operated a time, and this source would
be operated instead of the Knudsen
3260 only if needed (i.e., only one
would be in continuous operation
during the cruise).
Multi-Beam Sonar (Simrad EM120)—
The hull-mounted multi-beam sonar
would be operated continuously during
the cruise. This instrument operates at
a frequency of 12 kHz, has an estimated
maximum source energy level of 242 dB
re 1mPa (rms), and emits a very narrow
(<2°) beam fore to aft and 150° in crosstrack. The multi-beam system emits a
series of nine consecutive 15 ms pulses.
Acoustic Doppler Current Profiler
(ADCP Teledyne RDI VM–150)—The
hull-mounted ADCP would be operated
continuously throughout the cruise. The
ADCP operates at a frequency of 150
kHz with an estimated acoustic output
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100 ...................
190 dB
147.
(482.3 ft).
15.
(49.2 ft).
10.
(32.8 ft).
294.
(964.6 ft).
30.
(98.4 ft).
20.
(65.6 ft).
level at the source of 223.6 dB re 1mPa
(rms). Sound energy from the ADCP is
emitted as a 30° conically-shaped beam.
Acoustic Doppler Current Profiler
(ADCP Ocean Surveyor OS–38)—The
characteristics of this backup hullmounted ADCP unit are similar to the
Teledyne VM–150 and would be
continuously operated.
Acoustic Locator (Pinger)—An
acoustic locator (i.e., pinger) would be
deployed when using the SmithMcIntyre grab sampler and multi-corer
(Mega-corer) to enable these devices to
be located in the event they become
detached from their lines. A pinger
typically operates at a frequency of 12
kHz, generates a 5 ms pulse per second,
and has an acoustical output of 162 dB
re 1mPa (rms). A maximum total of 30
samples would be obtained using these
devices and require approximately one
hour per sample; therefore, the pinger
would operate for a total of 30 hours.
Passive Instruments—During the
seismic survey in the Dumont d’Urville
Sea, a precession magnetometer and
Air-Sea gravity meter would be
deployed. In addition, numerous
(approximately 24) expendable
bathythermograph (XBTs) probes would
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also be released (and none would be
recovered) over the course of the cruise
to obtain temperature data necessary to
calculate sound velocity profiles used
by the multi-beam sonar.
Core and Dredge Sampling
The primary sampling goals involve
the acquisition of marine sediment cores
of various lengths up to 25 m (82 ft). It
is anticipated that up to 65 sediment
cores and grab samples and 12 rock
dredge samples would be collected as
summarized in Table 3 (Table 3 of the
IHA application). Each core or grab
sample would require approximately
one hour per sample. All cores and
dredges would be deployed using a steel
cable/winch system.
Approximately 75 m2 (807.3 ft2) of
seafloor would be disturbed by each of
four deployments of the dredge at three
different sites (resulting in a total of 900
m2 [9,687.5 ft2] of affected seafloor for
the project). The selection of the bottom
sampling locations and sampling
method would be based on observations
of the seafloor, subsurface reflectivity,
sediment type, and accessibility due to
ice and weather conditions. Bottom
sampling in the Mertz Glacier area
would be limited to strategically
selected locations including possible resampling at a previous core site.
TABLE 3—PROPOSED CORING AND
DREDGING ACTIVITIES IN THE DUMONT D’URVILLE SEA
Sampling device
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Smith-MycIntyre grab sampler
Multi-corer (Mega-corer) ........
Kasten corer (regular or
jumbo).
Jumbo piston corer ................
Box cage dredge ....................
Number of
deployments
10 to 15.
10 to 15.
20 to 25.
8 to 10.
10 to 12.
Limited sampling of rock material
would be conducted using a dredge that
would be towed along the seafloor for
short distances (approximately 50 m
[164 ft]) to collect samples of bedrock
and ice rafted debris. The available
dredges, which have openings of 0.5 to
1.5 m (1.6 to 4.9 ft), would be deployed
on rocky substrates. The locations of the
proposed dredge sites are limited to the
inner shelf (southern) perimeter of three
areas: The Mertz Trough and two
regions along the Sabrina Coast. Final
selection of dredge sites will include
review to ensure that the seamounts or
corals in the area are avoided (AOA,
2011).
The Commission for the Conservation
of Antarctic Marine Living Resources
(CCAMLR) has adopted conservation
measures (i.e., 22–06, 22–07, and 22–09)
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to protect vulnerable marine ecosystems
(VME), which include seamounts,
hydrothermal vents, cold water corals,
and sponge fields. The conservation
measure 22–07 includes mitigation and
reporting requirements if VME are
encountered. The science team would
follow these requirements (see
Attachment C of the IHA application) if
VME’s are encountered while sampling
the sea bottom.
In addition, a camera and towed video
system would be deployed at up to 25
sites. This device would lightly touch
the seafloor to establish a baseline and
rise to an optimum elevation to obtain
the desired images.
Water Sampling and Current
Measurements
High-resolution conductivity, depth,
and temperature (CTD) measurements
would be collected to characterize the
summer regional water mass
stratification and circulation, and the
meridional exchange of waters between
the oceanic and shelf regimes. These
physical measurements would involve
approximately SeaBird CTD system
casts including the use of a lowered
ADCP (LADCP).
The LADCP would consist of two
Teledyne RDI Workhorse Monitor
ADCPs mounted on the CTD/rosette
frame and one oriented upward and the
other downward. The LADCP and frame
would be raised and lowered by cable
and winch. The LADCPs would operate
at a frequency of 307.2 kHz, with an
estimated output acoustic pressure
along each 4 beams of 216.3 dB re 1mPa
at 1 m. The beams are angled at 20
degrees from the centerline of the ADCP
head, with a beam angle of 4 degrees for
the individual beams. Typical pulse
duration is 5.7 ms, with a typical
repetition rate of 1.75 s. The upward
and downward-looking ADCPs are
operated in master-salve mode so that
only one head pings at a time. The
LADCP would be operated
approximately one hour at every CTD/
rosette station (maximum of 100
stations) for a total of 100 hours of
operation.
These instruments would be used to
profile the full water column for
temperature, salinity (conductivity),
dissolved oxygen and currents at a
series of transects in the study area.
Discrete water samples would be
collected for salinity and dissolved
oxygen to monitor CTD/rosette
performance, and for oxygen isotopes to
assess meltwater content. Water samples
would also be collected for development
and interpretation of marine sediment
proxies using Niskin bottles.
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469
Observations of the thermal structure
along other portions of the cruise track
would be made using an underway CTD
system and XBTs while the seafloor is
swath-mapped. The number and
spacing of stations would be adjusted
according to ocean features discovered
through multi-beam swath mapping and
the sea ice conditions. If portions of the
study area are inaccessible to the NBP,
a contingency sampling focused on the
inflows of MDCW would be pursued in
adjacent shelf troughs.
It is noted that underway ADCP on
the Palmer can, under ideal conditions,
obtain profiles of ocean currents to
depths greater than 800 m (2,624.7 ft).
On continental shelves where depths
may be less than the range of the ADCP,
the underway profiles cannot resolve
the deepest 15% of the water column
due to side lobe reflections from the
bottom which contaminate the water
column Doppler returns. For a depth of
800 m, expected in the MCDW, currents
in the lower 120 m (393.7 ft) could not
be measured by the ship ADCP;
therefore, the lowered ADCP can
provide accurate current profiles to
within a few meters of the bottom and
provide complete coverage of the
velocity field at each CTD station.
Instrumentation Moorings
Four instrumented moorings would
be deployed during the proposed cruise
to measure current, temperature, and
salinity (conductivity) continuously.
Two of the moorings would be deployed
for approximately one month (shortterm moorings) and two moorings
would be deployed for approximately
one year (long-term moorings). The two
short-term moorings and one long-term
mooring would include ADCP paired
with CTD recorders, and additional
intermediate T (i.e., temperature)
recorders. The characteristics of the
ADCP units deployed on the moorings
are similar to the Teledyne VM–150; the
moored ADCPs operate at frequencies of
75 kHz (one unit) and 300 kHz (two
units). The fourth mooring would be
equipped with sediment traps, a CTD
recorder and intermediate T recorders,
and be deployed for approximately one
year (long-term mooring). The two longterm moorings would be retrieved
approximately one year later by a U.S.
Arctic Program (USAP) vessel or
collaborators from other countries.
Subject to sea ice conditions, these
moorings would preferably be placed in
front of Totten Glacier, but otherwise as
close as possible inside adjacent crossshelf troughs. If access to the inner shelf
is not allowed by sea ice conditions we
would attempt mooring deployments
within the outer shelf close to the
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tkelley on DSK3SPTVN1PROD with NOTICES2
troughs mouth, where the Totten Glacier
is more directly connected to inflows
from the oceanic domain offshore. The
two long-term moorings would be
deployed within 16 km of each other.
The short-term moorings would be
within a few kilometers of each other
and no farther than 32 km (17.3 nmi)
from the long-term moorings. All
instruments would be kept at depths
below 250 m (820.2 ft) to minimize
damage or loss by icebergs.
The moorings would temporarily
attached to anchors and be recovered
using acoustic release mechanisms. The
mooring recovery process would be
similar regardless of mooring type or
when they would be retrieved. Locating
the moorings and releasing the moorings
from the steel railroad wheel anchors
(which would not be recovered) would
be accomplished by transmitting sound
over a period of several seconds. This is
done with an acoustic deck command
unit that sends a sequence of coded
pulses to the receiving units, the
acoustic releases, connected to the
mooring anchors. The acoustic releases
response to acknowledge the receipt of
commands from the deck unit is by
transmitting a short sequence of pulses
back. Both of the acoustic units
(onboard deck unit and moored
releases) operate at frequencies between
approximately 7 and 15 kHz. The beam
pattern is approximately
omnidirectional. The acoustic source
level is less than 192 dB re 1mPa at
1 m.
In addition to the U.S. moorings
described above, three new moorings
would be deployed on behalf of
Australia’s national science agency the
Commonwealth of Scientific and
Industrial Research Organisation
(CSIRO) Physical Oceanography group
in the Totten Glacier region by the
project team. These moorings would be
retrieved approximately one year later
by collaborators from other countries.
Also, during this cruise, three CSIRO
moorings that were deployed over a year
ago in the western outlet of the MertzNinnis Trough would be recovered. The
recovery process and acoustic sources
described above for the U.S. moorings
would be used for recovery of the
CSIRO moorings.
Icebreaking
Icebreaking is considered by NMFS to
be a continuous sound and NMFS
estimates that harassment occurs when
marine mammals are exposed to
continuous sounds at a received sound
level of 120 dB SPL or above. Potential
takes of marine mammals may ensue
from icebreaking activity in which the
Palmer is expected to engage in
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Antarctic waters (i.e., along the George
V and Oates Coast of East Antarctica,
>65° South, between 140° and 165°
East). While breaking ice, the noise from
the ship, including impact with ice,
engine noise, and propeller cavitation,
will exceed 120 dB (rms) continuously.
If icebreaking does occur in Antarctic
waters, NMFS, NSF and ASC expect it
will occur during transit and nonseismic operations to gain access to
coring, dredging, or other sampling
locations and not during seismic airgun
operations. The research activities and
associated contingencies are designed to
avoid areas of heavy sea ice condition.
The buffer zone (160 dB [rms]) for the
marine mammal Level B harassment
threshold during the proposed activities
is greater than the calculated radius
during icebreaking. Therefore, if the
Palmer breaks ice during seismic
operations within the Antarctic waters
(within the Dumont d’Urville Sea or
other areas of the Southern Ocean), the
more conservative and larger radius
(i.e., that for seismic operations) will be
used and supercede the buffer zone for
icebreaking.
In 2008, acousticians from Scripps
Institution of Oceanography Marine
Physical Laboratory and University of
New Hampshire Center for Coastal and
Ocean Mapping conducted
measurements of SPLs of the Healy
icebreaking under various conditions
(Roth and Schmidt, 2010). The results
indicated that the highest mean SPL
(185 dB) was measured at survey speeds
of 4 to 4.5 kts in conditions of 5/10 ice
and greater. Mean SPL under conditions
where the ship was breaking heavy ice
by backing and ramming was actually
lower (180 dB). In addition, when
backing and ramming, the vessel is
essentially stationary, so the ensonified
area is limited for a short period (on the
order of minutes to tens of minutes) to
the immediate vicinity of the vessel
until the ship breaks free and once again
makes headway.
The 120 dB received sound level
radius around the Healy while
icebreaking was estimated by
researchers (USGS, 2010). Using a
spherical spreading model, a source
level of 185 dB decays to 120 dB in
about 1,750 m (5,741.5 ft). This model
is corroborated by Roth and Schmidt
(2010). Therefore, as the ship travels
through the ice, a watch 3,500 m
(11,482.9 ft) wide would be subject to
sound levels greater than or equal to 120
dB. This results in potential exposure of
3,500 km2 (1,020.4 nmi2) to sounds
greater than or equal to 120 dB from
icebreaking.
Data characterizing the sound levels
generated by icebreaking activities
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conducted by the Palmer are not
available; therefore, data for noise
generating from an icebreaking vessel
such as the U.S. Coast Guard Cutter
(USCGC) Healy will be used as a proxy.
It is noted that the Palmer is a smaller
vessel and has less icebreaking
capability than the U.S. Coast Guard’s
other polar icebreakers, being only
capable of breaking ice up to 1 m thick
at speeds of 3 kts (5.6 km/hr or 3 nmi).
Therefore, the sound levels that may be
generated by the Palmer are expected to
be lower than the conservative levels
estimated and measured for the Healy.
Researchers will work to minimize time
spent breaking ice as science operations
are more difficult to conduct in icy
conditions since the ice noise degrades
the quality of the seismic and ADCP
data and time spent breaking ice takes
away from time supporting scientific
research. Logistically, if the vessel were
in heavy ice conditions, researchers
would not tow the airgun array and
streamer, as this would likely damage
equipment and generate noisy data. It is
possible that the seismic survey can be
performed in low ice conditions if the
Palmer could generate an open path
behind the vessel.
Because the Palmer is not rated to
break multi-year ice routinely,
operations generally avoid transiting
through older ice (i.e., 2 years or older,
thicker than 1 m). If sea ice is
encountered during the cruise, it is
anticipated the Palmer will proceed
primarily through one year sea ice, and
possibly some new, very thin ice, and
would follow leads wherever possible.
Satellite imagery from the Totten region
documents that sea ice is at its
minimum extent during the month of
February. The most recent image for the
region, from November 21, 2013, shows
that the sea ice is currently breaking up,
with a significant coastal lead of open
water. Based on a maximum sea ice
extent of 250 km (135 nmi) and
estimating that NSF and ASC will
transit to the innermost shelf and back
into open water twice, a round trip
transit in each of the potential work
regions, NSF and ASC estimate that the
Palmer will actively break ice up to a
distance of 1,000 km (540 nmi). Based
on a ship’s speed of 5 kts under
moderate ice conditions, this distance
represents approximately 108 hrs of
icebreaking operations. It is noted that
typical transit through areas primarily
open water and containing brash ice or
pancake ice will not be considered
icebreaking.
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Dates, Duration, and Specified
Geographic Region
The proposed project and survey sites
are located in selected regions of the
Dumont d’Urville Sea in the Southern
Ocean off the coast of East Antarctica
and focus on the Totten Glacier and
Moscow University Ice Shelf, located on
the Sabrina Coast, from greater than
approximately 64° South and between
approximately 95 to 135° East (see
Figure 2 of the IHA application), and the
Mertz Glacier and Cook Ice Shelf
systems located on the George V and
Oates Coast, from greater than
approximately 65° South and between
approximately 140 to 165° East in
International Waters. The proposed
study sites are characterized by heavy
ice cover, with a seasonal break-up in
the ice that structures biological
patterns. The proposed studies would
occur in both areas, or entirely in one
or the other, depending on ice
conditions. Figure 3 of the IHA
application illustrates the limited
detailed bathymetry of the two study
areas. Ice conditions encountered
during the previous surveys in the
region limited the area where
bathymetric data could be collected.
Water depths in the survey area range
from approximately 100 to 1,000 m, and
possibly exceeding 1,000 m in some
areas. There is limited information on
the depths in the study area and
therefore more detailed information on
bathymetry is not available. Figures 2
and 3 of the IHA application illustrate
the limited available detailed
bathymetry of the two proposed study
areas due to ice conditions encountered
during previous surveys in the region.
The proposed seismic survey would be
within an area of approximately 5,628
km2 (1,640.9 nmi2). This estimate is
based on the maximum number of
kilometers for the seismic survey (2,800
km) times the predicted rms radii (m)
based on modeling and empirical
measurements (assuming 100% use of
the two 105 in3 GI airguns in 100 to
1,000 m water depths) which was
calculated to be 1,005 m (3,297.2 ft).
The icebreaking will occur, as
necessary, between approximately 66 to
70° South and between 140 to 165° East.
The total distance in the region of the
vessel will travel include the proposed
seismic survey and transit to dredging
or sampling locations and will represent
approximately 5,600 km (3,023.8 nmi).
Based on a maximum sea ice extent of
250 km (135 nmi) and estimating that
NSF and ASC will transit to the
innermost shelf and back into open
water twice, a round trip transit in each
of the potential work regions, NSF and
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ASC estimate that the Palmer will
actively break ice up to a distance of
1,000 km (540 nmi). Based on a ship’s
speed of 5 kts under moderate ice
conditions, this distance represents
approximately 108 hrs of icebreaking
operations.
The Palmer is expected to depart from
Hobart, Tasmania on approximately
January 29, 2014 and arrive at Hobart,
Tasmania on approximately March 16,
2014. Research operations would be
over a span of 45-days, including to and
from port. Ice-free or very low
concentrations of sea ice are required in
order to collect high quality seismic
data and not impede passage of the
vessel between sampling locations. This
requirement restricts the cruise to
operating in mid to late austral summer
when the ice concentrations are
typically the lowest. Some minor
deviation from this schedule is possible,
depending on logistics and weather (i.e.,
the cruise may depart earlier or be
extended due to poor weather; there
could be additional days of seismic
operations if collected data are deemed
to be of substandard quality).
Description of the Marine Mammals in
the Area of the Proposed Specified
Activity
The marine mammals that generally
occur in the proposed action area belong
to three taxonomic groups: Mysticetes
(baleen whales), odontocetes (toothed
whales), and pinnipeds (seals and sea
lions). The marine mammal species that
potentially occur within the Southern
Ocean in proximity to the proposed
action area in the Dumont d’Urville Sea
include 28 species of cetaceans and 6
species of pinnipeds.
The Dumont d’Urville Sea may be a
feeding ground for many of these marine
mammals. Many of the species that may
be potentially present in the study area
seasonally migrate to higher latitudes
along the east coast of Antarctica. In
general, most species (except for the
killer whale) migrate north in the
middle of the austral winter and return
to Antarctica in the early austral
summer. Some species, particularly
Antarctic minke (Balaenoptera
bonaerensis) and killer whales (Orcinus
orca), are expected to be present in
higher concentrations along the ice edge
(SCAR, 2002). The 6 species of
pinnipeds that are found in the
Southern Ocean and which may be
present in the proposed study area
include the crabeater (Lebodon
carcinophagus), leopard (Hydrurga
leptonyx), Wedell (Leptonychotes
weddellii), Ross (Ommatophoca rossii),
southern elephant (Mirounga leonina),
and Antarctic fur seal (Arctocephalus
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471
gazella). Many of these pinniped species
breed on either the pack ice or subAntarctic islands. Since the southern
elephant seal and Antarctic fur seal
haul-outs and rookeries are located on
sub-Antarctic islands and prefer
beaches, they are more common north of
the seasonally shifting pack ice found in
the proposed study area; therefore, these
two species have not been considered
further. Marine mammal species listed
as endangered under the U.S.
Endangered Species Act of 1973 (ESA;
16 U.S.C. 1531 et seq.), includes the
southern right (Eubalaena australis),
humpback (Megaptera novaeangliae),
sei (Balaenoptera borealis), fin
(Balaenoptera physalus), blue
(Balaenoptera musculus), and sperm
(Physeter macrocephalus) whale. Of
those endangered species, the
humpback, sei, fin, blue, and sperm
whale are likely to be encountered in
the proposed survey area.
Various national Antarctic research
programs along the coast of East
Antarctica have conducted scientific
cruises that included data on marine
mammal sightings. These observations
were made primarily between 30° East
and 170° East and north to 60° South.
The reported cetacean sightings are
summarized in Tables 5 to 7 of the IHA
application. For pinnipeds, observations
made during a scientific cruise over a
13-day period in East Antarctica are
summarized in Table 8 of the IHA
application. These observations were
made below 60° South and between
110° East to 165° East and include
sightings of individual animals in the
water as well as individuals that were
hauled-out (i.e., resting on the surface of
the sea ice).
Records from the International
Whaling Commission’s Southern Ocean
Whale and Ecosystem Research (IWC–
SOWER) circumpolar cruises were also
considered. In addition to the 14 species
known to occur in the Dumont d’Urville
Sea of the Southern Ocean, there are 18
cetacean species with ranges that are
known to occur in the sub-Antarctic
waters of the study area which may also
feed and/or migrate to the Southern
Ocean during the austral summer, these
include the southern right, pygmy right
(Caperea marginata), Bryde’s
(Balaenoptera brydei), dwarf minke
(Balaenoptera acutorostrata spp.),
pygmy blue (Balaenoptera musculus
brevicauda), pygmy dwarf sperm whale
(Kogia breviceps), Arnoux’s beaked
(Berardius arnuxii), Blainville’s beaked
whale (Mesoplodon densirostris),
Cuvier’s beaked (Ziphius cavirostris),
Shepherd’s beaked (Tasmacetus
shepherdi), Southern bottlenose
(Hyperoodon planifrons), Andrew’s
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beaked (Mesoplodon bowdoini),
Hector’s beaked (Mesoplodon hectori),
Gray’s beaked (Mesoplodon grayi),
strap-toothed beaked (Mesoplodon
layardii), spade-toothed beaked
(Mesoplodon traversii), southern right
whale dolphin (Lissodelphis peronii),
Dusky (Lagenorhynchus obscurus), and
bottlenose dolphin (Tursiops truncatus).
However, these species have not been
sighted and are not expected to occur
where the proposed activities would
take place. These species are not
considered further in this document.
Table 4 (below) presents information on
the abundance, distribution, population
status, conservation status, and
population trend of the species of
marine mammals that may occur in the
proposed study area during February to
March 2014.
TABLE 4—THE HABITAT, REGIONAL ABUNDANCE, AND CONSERVATION STATUS OF MARINE MAMMALS THAT MAY OCCUR
IN OR NEAR THE PROPOSED LOW-ENERGY SEISMIC SURVEY AREA IN THE ANTARCTIC AREA OF THE SOUTHERN OCEAN
[See text and Tables 4 in NSF and ASC’s application for further details]
Habitat
Population estimate
ESA 1
MMPA 2
Coastal, pelagic ...................
8,000 3 to 15,000 4 ................
EN .......
D .........
Increasing.
Coastal, pelagic ...................
NA ........................................
NL .......
NC .......
NA.
Pelagic, nearshore waters,
and banks.
35,000 to 40,000 3—Worldwide.
9,484 5—Scotia Sea and
Antarctica Peninsula.
NA ........................................
EN .......
D .........
Increasing.
NL .......
NC .......
NA.
NL .......
NC .......
Stable.
NL .......
NC .......
NA.
Species
Mysticetes:
Southern right whale
(Eubalaena australis).
Pygmy right whale
(Caperea marginata).
Humpback whale
(Megaptera
novaeangliae).
Population trend
Pelagic and coastal ..............
Bryde’s whale
(Balaenoptera brydei).
Sei whale (Balaenoptera
borealis).
Fin whale (Balaenoptera
physalus).
tkelley on DSK3SPTVN1PROD with NOTICES2
Dwarf minke whale
(Balaenoptera
acutorostrata sub-species).
Antarctic minke whale
(Balaenoptera
bonaerensis).
Pelagic and coastal ..............
Several 100,000 3—Worldwide.
18,125 5—Scotia Sea and
Antarctica Peninsula.
NA ........................................
Primarily offshore, pelagic ....
80,000 3—Worldwide ............
EN .......
D .........
NA.
Continental slope, pelagic ....
EN .......
D .........
NA.
Blue whale
(Balaenoptera
musculus).
Odontocetes:
Sperm whale (Physeter
macrocephalus).
Pygmy sperm whale
(Kogia breviceps).
Arnoux’s beaked whale
(Berardius arnuxii).
Blainville’s beaked
whale (Mesoplodon
densirostris).
Cuvier’s beaked whale
(Ziphius cavirostris).
Shepherd’s beaked
whale (Tasmacetus
shepherdi).
Southern bottlenose
whale (Hyperoodon
planifrons).
Andrew’s beaked whale
(Mesoplodon
bowdoini).
Hector’s beaked whale
(Mesoplodon hectori).
Gray’s beaked whale
(Mesoplodon grayi).
Strap-toothed beaked
whale (Mesoplodon
layardii).
Spade-toothed beaked
whale (Mesoplodon
traversii).
Pelagic, shelf, coastal ..........
140,000 3—Worldwide ..........
4,672 5—Scotia Sea and
Antarctica Peninsula.
8,000 to 9,000 3—Worldwide
1,700 6—Southern Ocean ....
EN .......
D .........
NA.
EN .......
D .........
NA.
Pelagic, slope .......................
360,000 3—Worldwide ..........
9,500 3—Antarctic .................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
500,000 3—South of Antarctic Convergence.
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
Pelagic .................................
NA ........................................
NL .......
NC .......
NA.
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Pelagic, ice floes ..................
Pelagic, deep sea ................
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
TABLE 4—THE HABITAT, REGIONAL ABUNDANCE, AND CONSERVATION STATUS OF MARINE MAMMALS THAT MAY OCCUR
IN OR NEAR THE PROPOSED LOW-ENERGY SEISMIC SURVEY AREA IN THE ANTARCTIC AREA OF THE SOUTHERN
OCEAN—Continued
[See text and Tables 4 in NSF and ASC’s application for further details]
Species
Habitat
Population estimate
ESA 1
MMPA 2
Killer whale (Orcinus
orca).
Pelagic, shelf, coastal, pack
ice.
NL .......
NC .......
NA.
Long-finned pilot whale
(Globicephala melas).
Bottlenose dolphin
(Tursiops truncatus).
Southern right whale
dolphin (Lissodelphis
peronii).
Dusky dolphin
(Lagenorhynchus
obscurus).
Hourglass dolphin
(Lagenorhynchus
cruciger).
Spectacled porpoise
(Phocoena dioptrica).
Pinnipeds:
Crabeater seal (Lobodon
carcinophaga).
Leopard seal (Hydrurga
leptonyx).
Ross seal
(Ommatophoca rossii).
Wedell seal
(Leptonychotes
weddellii).
Southern elephant seal
(Mirounga leonina).
Pelagic, shelf, coastal ..........
80,000 3—South of Antarctic
Convergence.
25,000 7—Southern Ocean ..
200,000 3 8—South of Antarctic Convergence.
>625,500 3—Worldwide ........
NL .......
NC .......
NA.
NL .......
NC .......
NA.
NA ........................................
NL .......
NC .......
NA.
Coastal, continental shelf
and slope.
NA ........................................
NL .......
NC .......
NA.
Pelatic, ice edge ..................
144,000 3 ..............................
NL .......
NC .......
NA.
Coastal, pelagic ...................
NA ........................................
NL .......
NC .......
NA.
Coastal, pack ice .................
5,000,000 to 15,000,000 3 9 ..
NL .......
NC .......
Increasing.
Pack ice, sub-Antarctic islands.
Pack ice, smooth ice floes,
pelagic.
Fast ice, pack ice, sub-Antarctic islands.
220,000 to 440,000 3 10 ........
NL .......
NC .......
NA.
130,000 3 ..............................
NL .......
NC .......
NA.
500,000 to 1,000,000 3 11 .....
NL .......
NC .......
NA.
Coastal, pelagic, sub-Antarctic waters.
640,000 12 to 650,000 3 ........
NL .......
NC .......
Shelf, rocky habitats ............
1,600,000 13 to 3,000,000 3 ..
NL .......
NC .......
Decreasing, increasing or
stable depending on
breeding population.
Increasing.
Antarctic fur seal
(Arctocephalus
gazella).
Offshore, inshore, coastal,
estuaries.
Pelagic .................................
Population trend
tkelley on DSK3SPTVN1PROD with NOTICES2
NA = Not available or not assessed.
1 U.S. Endangered Species Act: EN = Endangered, T = Threatened, DL = Delisted, NL = Not listed.
2 U.S. Marine Mammal Protection Act: D = Depleted, S = Strategic, NC = Not Classified.
3 Jefferson et al., 2008.
4 Kenney, 2009.
5 Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR) survey area (Reilly et al., 2004).
6 Sears and Perrin, 2009.
7 Ford, 2009.
8 Olson, 2009.
9 Bengston, 2009.
10 Rogers, 2009.
11 Thomas and Terhune, 2009.
12 Hindell and Perrin, 2009.
13 Arnould, 2009.
Refer to sections 3 and 4 of NSF and
ASC’s IHA application for detailed
information regarding the abundance
and distribution, population status, and
life history and behavior of these other
marine mammal species and their
occurrence in the proposed project area.
The IHA application also presents how
NSF and ASC calculated the estimated
densities for the marine mammals in the
proposed survey area. NMFS has
reviewed these data and determined
them to be the best available scientific
information for the purposes of the
proposed IHA.
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Potential Effects on Marine Mammals
Acoustic stimuli generated by the
operation of the airguns, which
introduce sound into the marine
environment, may have the potential to
cause Level B harassment of marine
mammals in the proposed survey area.
The effects of sounds from airgun
operations might include one or more of
the following: Tolerance, masking of
natural sounds, behavioral disturbance,
temporary or permanent hearing
impairment, or non-auditory physical or
physiological effects (Richardson et al.,
1995; Gordon et al., 2004; Nowacek et
al., 2007; Southall et al., 2007).
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Permanent hearing impairment, in the
unlikely event that it occurred, would
constitute injury, but temporary
threshold shift (TTS) is not an injury
(Southall et al., 2007). Although the
possibility cannot be entirely excluded,
it is unlikely that the proposed project
would result in any cases of temporary
or permanent hearing impairment, or
any significant non-auditory physical or
physiological effects. Based on the
available data and studies described
here, some behavioral disturbance is
expected. A more comprehensive
review of these issues can be found in
the ‘‘Programmatic Environmental
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Impact Statement/Overseas
Environmental Impact Statement
prepared for Marine Seismic Research
that is funded by the National Science
Foundation and conducted by the U.S.
Geological Survey’’ (NSF/USGS, 2011).
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Tolerance
Richardson et al. (1995) defines
tolerance as the occurrence of marine
mammals in areas where they are
exposed to human activities or manmade noise. In many cases, tolerance
develops by the animal habituating to
the stimulus (i.e., the gradual waning of
responses to a repeated or ongoing
stimulus) (Richardson, et al., 1995;
Thorpe, 1963), but because of ecological
or physiological requirements, many
marine animals may need to remain in
areas where they are exposed to chronic
stimuli (Richardson, et al., 1995).
Numerous studies have shown that
pulsed sounds from airguns are often
readily detectable in the water at
distances of many kilometers. Several
studies have shown that marine
mammals at distances more than a few
kilometers from operating seismic
vessels often show no apparent
response. That is often true even in
cases when the pulsed sounds must be
readily audible to the animals based on
measured received levels and the
hearing sensitivity of the marine
mammal group. Although various
baleen whales and toothed whales, and
(less frequently) pinnipeds have been
shown to react behaviorally to airgun
pulses under some conditions, at other
times marine mammals of all three types
have shown no overt reactions. The
relative responsiveness of baleen and
toothed whales are quite variable.
Masking
The term masking refers to the
inability of a subject to recognize the
occurrence of an acoustic stimulus as a
result of the interference of another
acoustic stimulus (Clark et al., 2009).
Introduced underwater sound may,
through masking, reduce the effective
communication distance of a marine
mammal species if the frequency of the
source is close to that used as a signal
by the marine mammal, and if the
anthropogenic sound is present for a
significant fraction of the time
(Richardson et al., 1995).
The airguns for the proposed lowenergy seismic survey have dominant
frequency components of 2 to 188 Hz.
This frequency range fully overlaps the
lower part of the frequency range of
odontocete calls and/or functional
hearing (full range about 150 Hz to 180
kHz). Airguns also produce a small
portion of their sound at mid and high
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frequencies that overlap most, if not all,
frequencies produced by odontocetes.
While it is assumed that mysticetes can
detect acoustic impulses from airguns
and vessel sounds (Richardson et al.,
1995a), sub-bottom profilers, pingers,
and most of the multi-beam
echosounders would likely be
detectable by some mysticetes based on
presumed mysticete hearing sensitivity.
Odontocetes are presumably more
sensitive to mid to high frequencies
produced by the mulit-beam
echosounders, sub-bottom profilers, and
pingers than to the dominant low
frequencies produced by the airguns
and vessel. A more comprehensive
review of the relevant background
information for odontocetes appears in
Section 3.6.4.3, Section 3.7.4.3 and
Appendix E of the NSF/USGS PEIS
(2011).
Masking effects of pulsed sounds
(even from large arrays of airguns) on
marine mammal calls and other natural
sounds are expected to be limited.
Because of the intermittent nature and
low duty cycle of seismic airgun pulses,
animals can emit and receive sounds in
the relatively quiet intervals between
pulses. However, in some situations,
reverberation occurs for much or the
entire interval between pulses (e.g.,
Simard et al., 2005; Clark and Gagnon,
2006) which could mask calls. Some
baleen and toothed whales are known to
continue calling in the presence of
seismic pulses, and their calls can
usually be heard between the seismic
pulses (e.g., Richardson et al., 1986;
McDonald et al., 1995; Greene et al.,
1999; Nieukirk et al., 2004; Smultea et
al., 2004; Holst et al., 2005a,b, 2006; and
Dunn and Hernandez, 2009). However,
Clark and Gagnon (2006) reported that
fin whales in the North Atlantic Ocean
went silent for an extended period
starting soon after the onset of a seismic
survey in the area. Similarly, there has
been one report that sperm whales
ceased calling when exposed to pulses
from a very distant seismic ship (Bowles
et al., 1994). However, more recent
studies found that they continued
calling in the presence of seismic pulses
(Madsen et al., 2002; Tyack et al., 2003;
Smultea et al., 2004; Holst et al., 2006;
and Jochens et al., 2008). Dilorio and
Clark (2009) found evidence of
increased calling by blue whales during
operations by a lower-energy seismic
source (i.e., sparker). Dolphins and
porpoises commonly are heard calling
while airguns are operating (e.g.,
Gordon et al., 2004; Smultea et al., 2004;
Holst et al., 2005a, b; and Potter et al.,
2007). The sounds important to small
odontocetes are predominantly at much
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higher frequencies than are the
dominant components of airgun sounds,
thus limiting the potential for masking.
Pinnipeds have the most sensitive
hearing and/or produce most of their
sounds in frequencies higher than the
dominant components of airgun sound,
but there is some overlap in the
frequencies of the airgun pulses and the
calls. However, the intermittent nature
of airgun pules presumably reduces the
potential for masking.
Marine mammals are thought to be
able to compensate for masking by
adjusting their acoustic behavior
through shifting call frequencies,
increasing call volume, and increasing
vocalization rates. For example blue
whales are found to increase call rates
when exposed to noise from seismic
surveys in the St. Lawrence Estuary
(Dilorio and Clark, 2009). The North
Atlantic right whales (Eubalaena
glacialis) exposed to high shipping
noise increased call frequency (Parks et
al., 2007), while some humpback
whales respond to low-frequency active
sonar playbacks by increasing song
length (Miller et al., 2000). In general,
NMFS expects the masking effects of
seismic pulses to be minor, given the
normally intermittent nature of seismic
pulses.
Behavioral Disturbance
Marine mammals may behaviorally
react to sound when exposed to
anthropogenic noise. Disturbance
includes a variety of effects, including
subtle to conspicuous changes in
behavior, movement, and displacement.
Reactions to sound, if any, depend on
species, state of maturity, experience,
current activity, reproductive state, time
of day, and many other factors
(Richardson et al., 1995; Wartzok et al.,
2004; Southall et al., 2007; Weilgart,
2007). These behavioral reactions are
often shown as: Changing durations of
surfacing and dives, number of blows
per surfacing, or moving direction and/
or speed; reduced/increased vocal
activities; changing/cessation of certain
behavioral activities (such as socializing
or feeding); visible startle response or
aggressive behavior (such as tail/fluke
slapping or jaw clapping); avoidance of
areas where noise sources are located;
and/or flight responses (e.g., pinnipeds
flushing into the water from haul-outs
or rookeries). If a marine mammal does
react briefly to an underwater sound by
changing its behavior or moving a small
distance, the impacts of the change are
unlikely to be significant to the
individual, let alone the stock or
population. However, if a sound source
displaces marine mammals from an
important feeding or breeding area for a
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
prolonged period, impacts on
individuals and populations could be
significant (e.g., Lusseau and Bejder,
2007; Weilgart, 2007).
The biological significance of many of
these behavioral disturbances is difficult
to predict, especially if the detected
disturbances appear minor. However,
the consequences of behavioral
modification could be expected to be
biologically significant if the change
affects growth, survival, and/or
reproduction. Some of these significant
behavioral modifications include:
• Change in diving/surfacing patterns
(such as those thought to be causing
beaked whale stranding due to exposure
to military mid-frequency tactical
sonar);
• Habitat abandonment due to loss of
desirable acoustic environment; and
• Cessation of feeding or social
interaction.
The onset of behavioral disturbance
from anthropogenic noise depends on
both external factors (characteristics of
noise sources and their paths) and the
receiving animals (hearing, motivation,
experience, demography) and is also
difficult to predict (Richardson et al.,
1995; Southall et al., 2007). Given the
many uncertainties in predicting the
quantity and types of impacts of noise
on marine mammals, it is common
practice to estimate how many
mammals would be present within a
particular distance of industrial
activities and/or exposed to a particular
level of sound. In most cases, this
approach likely overestimates the
numbers of marine mammals that would
be affected in some biologicallyimportant manner.
Baleen Whales—Baleen whales
generally tend to avoid operating
airguns, but avoidance radii are quite
variable (reviewed in Richardson et al.,
1995; Gordon et al., 2004). Whales are
often reported to show no overt
reactions to pulses from large arrays of
airguns at distances beyond a few
kilometers, even though the airgun
pulses remain well above ambient noise
levels out to much longer distances.
However, baleen whales exposed to
strong noise pulses from airguns often
react by deviating from their normal
migration route and/or interrupting
their feeding and moving away. In the
cases of migrating gray (Eschrichtius
robustus) and bowhead (Balaena
mysticetus) whales, the observed
changes in behavior appeared to be of
little or no biological consequence to the
animals (Richardson, et al., 1995). They
simply avoided the sound source by
displacing their migration route to
varying degrees, but within the natural
boundaries of the migration corridors.
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Studies of gray, bowhead, and
humpback whales have shown that
seismic pulses with received levels of
160 to 170 dB re 1 mPa (rms) seem to
cause obvious avoidance behavior in a
substantial fraction of the animals
exposed (Malme et al., 1986, 1988;
Richardson et al., 1995). In many areas,
seismic pulses from large arrays of
airguns diminish to those levels at
distances ranging from 4 to 15 km (2.2
to 8.1 nmi) from the source. A
substantial proportion of the baleen
whales within those distances may
show avoidance or other strong
behavioral reactions to the airgun array.
Subtle behavioral changes sometimes
become evident at somewhat lower
received levels, and studies have shown
that some species of baleen whales,
notably bowhead, gray, and humpback
whales, at times, show strong avoidance
at received levels lower than 160 to 170
dB re 1 mPa (rms).
Researchers have studied the
responses of humpback whales to
seismic surveys during migration,
feeding during the summer months,
breeding while offshore from Angola,
and wintering offshore from Brazil.
McCauley et al. (1998, 2000a) studied
the responses of humpback whales off
western Australia to a full-scale seismic
survey with a 16 airgun array (2,678 in3)
and to a single airgun (20 in3) with
source level of 227 dB re 1 mPa (p-p). In
the 1998 study, they documented that
avoidance reactions began at 5 to 8 km
(2.7 to 4.3 nmi) from the array, and that
those reactions kept most pods
approximately 3 to 4 km (1.6 to 2.2 nmi)
from the operating seismic boat. In the
2000 study, they noted localized
displacement during migration of 4 to 5
km (2.2 to 2.7 nmi) by traveling pods
and 7 to 12 km (3.8 to 6.5 nmi) by more
sensitive resting pods of cow-calf pairs.
Avoidance distances with respect to the
single airgun were smaller but
consistent with the results from the full
array in terms of the received sound
levels. The mean received level for
initial avoidance of an approaching
airgun was 140 dB re 1 mPa (rms) for
humpback pods containing females, and
at the mean closest point of approach
distance the received level was 143 dB
re 1 mPa (rms). The initial avoidance
response generally occurred at distances
of 5 to 8 km (2.7 to 4.3 nmi) from the
airgun array and 2 km (1.1 nmi) from
the single airgun. However, some
individual humpback whales, especially
males, approached within distances of
100 to 400 m (328 to 1,312 ft), where the
maximum received level was 179 dB re
1 mPa (rms).
Data collected by observers during
several seismic surveys in the
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475
Northwest Atlantic showed that sighting
rates of humpback whales were
significantly greater during non-seismic
periods compared with periods when a
full array was operating (Moulton and
Holst, 2010). In addition, humpback
whales were more likely to swim away
and less likely to swim towards a vessel
during seismic vs. non-seismic periods
(Moulton and Holst, 2010).
Humpback whales on their summer
feeding grounds in southeast Alaska did
not exhibit persistent avoidance when
exposed to seismic pulses from a 1.64–
L (100 in3) airgun (Malme et al., 1985).
Some humpbacks seemed ‘‘startled’’ at
received levels of 150 to 169 dB re 1
mPa. Malme et al. (1985) concluded that
there was no clear evidence of
avoidance, despite the possibility of
subtle effects, at received levels up to
172 dB re 1 mPa (rms). However,
Moulton and Holst (2010) reported that
humpback whales monitored during
seismic surveys in the Northwest
Atlantic had lower sighting rates and
were most often seen swimming away
from the vessel during seismic periods
compared with periods when airguns
were silent.
Studies have suggested that South
Atlantic humpback whales wintering off
Brazil may be displaced or even strand
upon exposure to seismic surveys (Engel
et al., 2004). The evidence for this was
circumstantial and subject to alternative
explanations (IAGC, 2004). Also, the
evidence was not consistent with
subsequent results from the same area of
Brazil (Parente et al., 2006), or with
direct studies of humpbacks exposed to
seismic surveys in other areas and
seasons. After allowance for data from
subsequent years, there was ‘‘no
observable direct correlation’’ between
strandings and seismic surveys (IWC,
2007: 236).
Reactions of migrating and feeding
(but not wintering) gray whales to
seismic surveys have been studied.
Malme et al. (1986, 1988) studied the
responses of feeding eastern Pacific gray
whales to pulses from a single 100 in3
airgun off St. Lawrence Island in the
northern Bering Sea. They estimated,
based on small sample sizes, that 50
percent of feeding gray whales stopped
feeding at an average received pressure
level of 173 dB re 1 mPa on an
(approximate) rms basis, and that 10
percent of feeding whales interrupted
feeding at received levels of 163 dB re
1 mPa (rms). Those findings were
generally consistent with the results of
experiments conducted on larger
numbers of gray whales that were
migrating along the California coast
(Malme et al., 1984; Malme and Miles,
1985), and western Pacific gray whales
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feeding off Sakhalin Island, Russia
(Wursig et al., 1999; Gailey et al., 2007;
Johnson et al., 2007; Yazvenko et al.,
2007a, b), along with data on gray
whales off British Columbia (Bain and
Williams, 2006).
Various species of Balaenoptera (blue,
sei, fin, and minke whales) have
occasionally been seen in areas
ensonified by airgun pulses (Stone,
2003; MacLean and Haley, 2004; Stone
and Tasker, 2006), and calls from blue
and fin whales have been localized in
areas with airgun operations (e.g.,
McDonald et al., 1995; Dunn and
Hernandez, 2009; Castellote et al.,
2010). Sightings by observers on seismic
vessels off the United Kingdom from
1997 to 2000 suggest that, during times
of good sightability, sighting rates for
mysticetes (mainly fin and sei whales)
were similar when large arrays of
airguns were shooting versus silent
(Stone, 2003; Stone and Tasker, 2006).
However, these whales tended to exhibit
localized avoidance, remaining
significantly further (on average) from
the airgun array during seismic
operations compared with non-seismic
periods (Stone and Tasker, 2006).
Castellote et al. (2010) reported that
singing fin whales in the Mediterranean
moved away from an operating airgun
array.
Ship-based monitoring studies of
baleen whales (including blue, fin, sei,
minke, and humpback whales) in the
Northwest Atlantic found that overall,
this group had lower sighting rates
during seismic vs. non-seismic periods
(Moulton and Holst, 2010). Baleen
whales as a group were also seen
significantly farther from the vessel
during seismic compared with nonseismic periods, and they were more
often seen to be swimming away from
the operating seismic vessel (Moulton
and Holst, 2010). Blue and minke
whales were initially sighted
significantly farther from the vessel
during seismic operations compared to
non-seismic periods; the same trend was
observed for fin whales (Moulton and
Holst, 2010). Minke whales were most
often observed to be swimming away
from the vessel when seismic operations
were underway (Moulton and Holst,
2010).
Data on short-term reactions by
cetaceans to impulsive noises are not
necessarily indicative of long-term or
biologically significant effects. It is not
known whether impulsive sounds affect
reproductive rate or distribution and
habitat use in subsequent days or years.
However, gray whales have continued to
migrate annually along the west coast of
North America with substantial
increases in the population over recent
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years, despite intermittent seismic
exploration (and much ship traffic) in
that area for decades (Appendix A in
Malme et al., 1984; Richardson et al.,
1995; Allen and Angliss, 2010). The
western Pacific gray whale population
did not seem affected by a seismic
survey in its feeding ground during a
previous year (Johnson et al., 2007).
Similarly, bowhead whales have
continued to travel to the eastern
Beaufort Sea each summer, and their
numbers have increased notably,
despite seismic exploration in their
summer and autumn range for many
years (Richardson et al., 1987; Allen and
Angliss, 2010). The history of
coexistence between seismic surveys
and baleen whales suggests that brief
exposures to sound pulses from any
single seismic survey are unlikely to
result in prolonged effects.
Toothed Whales—Little systematic
information is available about reactions
of toothed whales to noise pulses. Few
studies similar to the more extensive
baleen whale/seismic pulse work
summarized above have been reported
for toothed whales. However, there are
recent systematic studies on sperm
whales (e.g., Gordon et al., 2006;
Madsen et al., 2006; Winsor and Mate,
2006; Jochens et al., 2008; Miller et al.,
2009). There is an increasing amount of
information about responses of various
odontocetes to seismic surveys based on
monitoring studies (e.g., Stone, 2003;
Smultea et al., 2004; Moulton and
Miller, 2005; Bain and Williams, 2006;
Holst et al., 2006; Stone and Tasker,
2006; Potter et al., 2007; Hauser et al.,
2008; Holst and Smultea, 2008; Weir,
2008; Barkaszi et al., 2009; Richardson
et al., 2009; Moulton and Holst, 2010).
Seismic operators and PSOs on
seismic vessels regularly see dolphins
and other small toothed whales near
operating airgun arrays, but in general
there is a tendency for most delphinids
to show some avoidance of operating
seismic vessels (e.g., Goold, 1996a,b,c;
Calambokidis and Osmek, 1998; Stone,
2003; Moulton and Miller, 2005; Holst
et al., 2006; Stone and Tasker, 2006;
Weir, 2008; Richardson et al., 2009;
Barkaszi et al., 2009; Moulton and
Holst, 2010). Some dolphins seem to be
attracted to the seismic vessel and
floats, and some ride the bow wave of
the seismic vessel even when large
arrays of airguns are firing (e.g.,
Moulton and Miller, 2005). Nonetheless,
small toothed whales more often tend to
head away, or to maintain a somewhat
greater distance from the vessel, when a
large array of airguns is operating than
when it is silent (e.g., Stone and Tasker,
2006; Weir, 2008; Barry et al., 2010;
Moulton and Holst, 2010). In most
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cases, the avoidance radii for delphinids
appear to be small, on the order of one
km or less, and some individuals show
no apparent avoidance. Captive
bottlenose dolphins and beluga whales
(Delphinapterus leucas) exhibited
changes in behavior when exposed to
strong pulsed sounds similar in
duration to those typically used in
seismic surveys (Finneran et al., 2000,
2002, 2005). However, the animals
tolerated high received levels of sound
before exhibiting aversive behaviors.
Results of porpoises depend on
species. The limited available data
suggest that harbor porpoises (Phocoena
phocoena) show stronger avoidance of
seismic operations than do Dall’s
porpoises (Phocoenoides dalli) (Stone,
2003; MacLean and Koski, 2005; Bain
and Williams, 2006; Stone and Tasker,
2006). Dall’s porpoises seem relatively
tolerant of airgun operations (MacLean
and Koski, 2005; Bain and Williams,
2006), although they too have been
observed to avoid large arrays of
operating airguns (Calambokidis and
Osmek, 1998; Bain and Williams, 2006).
This apparent difference in
responsiveness of these two porpoise
species is consistent with their relative
responsiveness to boat traffic and some
other acoustic sources (Richardson et
al., 1995; Southall et al., 2007).
Most studies of sperm whales exposed
to airgun sounds indicate that the sperm
whale shows considerable tolerance of
airgun pulses (e.g., Stone, 2003;
Moulton et al., 2005, 2006a; Stone and
Tasker, 2006; Weir, 2008). In most cases
the whales do not show strong
avoidance, and they continue to call.
However, controlled exposure
experiments in the Gulf of Mexico
indicate that foraging behavior was
altered upon exposure to airgun sound
(Jochens et al., 2008; Miller et al., 2009;
Tyack, 2009). There are almost no
specific data on the behavioral reactions
of beaked whales to seismic surveys.
However, some northern bottlenose
whales (Hyperoodon ampullatus)
remained in the general area and
continued to produce high-frequency
clicks when exposed to sound pulses
from distant seismic surveys (Gosselin
and Lawson, 2004; Laurinolli and
Cochrane, 2005; Simard et al., 2005).
Most beaked whales tend to avoid
approaching vessels of other types (e.g.,
Wursig et al., 1998). They may also dive
for an extended period when
approached by a vessel (e.g., Kasuya,
1986), although it is uncertain how
much longer such dives may be as
compared to dives by undisturbed
beaked whales, which also are often
quite long (Baird et al., 2006; Tyack et
al., 2006). Based on a single observation,
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Aguilar-Soto et al. (2006) suggested that
foraging efficiency of Cuvier’s beaked
whales may be reduced by close
approach of vessels. In any event, it is
likely that most beaked whales would
also show strong avoidance of an
approaching seismic vessel, although
this has not been documented
explicitly. In fact, Moulton and Holst
(2010) reported 15 sightings of beaked
whales during seismic studies in the
Northwest Atlantic; seven of those
sightings were made at times when at
least one airgun was operating. There
was little evidence to indicate that
beaked whale behavior was affected by
airgun operations; sighting rates and
distances were similar during seismic
and non-seismic periods (Moulton and
Holst, 2010).
There are increasing indications that
some beaked whales tend to strand
when naval exercises involving midfrequency sonar operation are ongoing
nearby (e.g., Simmonds and LopezJurado, 1991; Frantzis, 1998; NOAA and
USN, 2001; Jepson et al., 2003;
Hildebrand, 2005; Barlow and Gisiner,
2006; see also the ‘‘Stranding and
Mortality’’ section in this notice). These
strandings are apparently a disturbance
response, although auditory or other
injuries or other physiological effects
may also be involved. Whether beaked
whales would ever react similarly to
seismic surveys is unknown. Seismic
survey sounds are quite different from
those of the sonar in operation during
the above-cited incidents.
Odontocete reactions to large arrays of
airguns are variable and, at least for
delphinids, seem to be confined to a
smaller radius than has been observed
for the more responsive of some
mysticetes. However, other data suggest
that some odontocete species, including
harbor porpoises, may be more
responsive than might be expected
given their poor low-frequency hearing.
Reactions at longer distances may be
particularly likely when sound
propagation conditions are conducive to
transmission of the higher frequency
components of airgun sound to the
animals’ location (DeRuiter et al., 2006;
Goold and Coates, 2006; Tyack et al.,
2006; Potter et al., 2007).
Pinnipeds—Pinnipeds are not likely
to show a strong avoidance reaction to
the airgun array. Visual monitoring from
seismic vessels has shown only slight (if
any) avoidance of airguns by pinnipeds,
and only slight (if any) changes in
behavior. In the Beaufort Sea, some
ringed seals avoided an area of 100 m
to (at most) a few hundred meters
around seismic vessels, but many seals
remained within 100 to 200 m (328 to
656 ft) of the trackline as the operating
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airgun array passed by (e.g., Harris et al.,
2001; Moulton and Lawson, 2002;
Miller et al., 2005.). Ringed seal (Pusa
hispida) sightings averaged somewhat
farther away from the seismic vessel
when the airguns were operating than
when they were not, but the difference
was small (Moulton and Lawson, 2002).
Similarly, in Puget Sound, sighting
distances for harbor seals (Phoca
vitulina) and California sea lions
(Zalophus californianus) tended to be
larger when airguns were operating
(Calambokidis and Osmek, 1998).
Previous telemetry work suggests that
avoidance and other behavioral
reactions may be stronger than evident
to date from visual studies (Thompson
et al., 1998).
During seismic exploration off Nova
Scotia, gray seals (Halichoerus grypus)
exposed to noise from airguns and
linear explosive charges did not react
strongly (J. Parsons in Greene et al.,
1985). Pinnipeds in both water and air,
sometimes tolerate strong noise pulses
from non-explosive and explosive
scaring devices, especially if attracted to
the area for feeding and reproduction
(Mate and Harvey, 1987; Reeves et al.,
1996). Thus pinnipeds are expected to
be rather tolerant of, or habituate to,
repeated underwater sounds from
distant seismic sources, at least when
the animals are strongly attracted to the
area.
Hearing Impairment and Other Physical
Effects
Exposure to high intensity sound for
a sufficient duration may result in
auditory effects such as a noise-induced
threshold shift—an increase in the
auditory threshold after exposure to
noise (Finneran, Carder, Schlundt, and
Ridgway, 2005). Factors that influence
the amount of threshold shift include
the amplitude, duration, frequency
content, temporal pattern, and energy
distribution of noise exposure. The
magnitude of hearing threshold shift
normally decreases over time following
cessation of the noise exposure. The
amount of threshold shift just after
exposure is called the initial threshold
shift. If the threshold shift eventually
returns to zero (i.e., the threshold
returns to the pre-exposure value), it is
called temporary threshold shift (TTS)
(Southall et al., 2007). Researchers have
studied TTS in certain captive
odontocetes and pinnipeds exposed to
strong sounds (reviewed in Southall et
al., 2007). However, there has been no
specific documentation of TTS let alone
permanent hearing damage, i.e.,
permanent threshold shift (PTS), in freeranging marine mammals exposed to
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477
sequences of airgun pulses during
realistic field conditions.
Temporary Threshold Shift—TTS is
the mildest form of hearing impairment
that can occur during exposure to a
strong sound (Kryter, 1985). While
experiencing TTS, the hearing threshold
rises and a sound must be stronger in
order to be heard. At least in terrestrial
mammals, TTS can last from minutes or
hours to (in cases of strong TTS) days.
For sound exposures at or somewhat
above the TTS threshold, hearing
sensitivity in both terrestrial and marine
mammals recovers rapidly after
exposure to the noise ends. Few data on
sound levels and durations necessary to
elicit mild TTS have been obtained for
marine mammals, and none of the
published data concern TTS elicited by
exposure to multiple pulses of sound.
Available data on TTS in marine
mammals are summarized in Southall et
al. (2007). Table 2 (above) presents the
estimated distances from the Palmer’s
airguns at which the received energy
level (per pulse, flat-weighted) would be
expected to be greater than or equal to
180 and 190 dB re 1 mPa (rms).
To avoid the potential for injury,
NMFS (1995, 2000) concluded that
cetaceans and pinnipeds should not be
exposed to pulsed underwater noise at
received levels exceeding 180 and 190
dB re 1 mPa (rms). NMFS believes that
to avoid the potential for Level A
harassment, cetaceans and pinnipeds
should not be exposed to pulsed
underwater noise at received levels
exceeding 180 and 190 dB re 1 mPa
(rms), respectively. The established 180
and 190 dB (rms) criteria are not
considered to be the levels above which
TTS might occur. Rather, they are the
received levels above which, in the view
of a panel of bioacoustics specialists
convened by NMFS before TTS
measurements for marine mammals
started to become available, one could
not be certain that there would be no
injurious effects, auditory or otherwise,
to marine mammals. NMFS also
assumes that cetaceans and pinnipeds
exposed to levels exceeding 160 dB re
1 mPa (rms) may experience Level B
harassment.
For toothed whales, researchers have
derived TTS information for
odontocetes from studies on the
bottlenose dolphin and beluga. The
experiments show that exposure to a
single impulse at a received level of 207
kPa (or 30 psi, p-p), which is equivalent
to 228 dB re 1 Pa (p-p), resulted in a 7
and 6 dB TTS in the beluga whale at 0.4
and 30 kHz, respectively. Thresholds
returned to within 2 dB of the preexposure level within 4 minutes of the
exposure (Finneran et al., 2002). For the
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one harbor porpoise tested, the received
level of airgun sound that elicited onset
of TTS was lower (Lucke et al., 2009).
If these results from a single animal are
representative, it is inappropriate to
assume that onset of TTS occurs at
similar received levels in all
odontocetes (cf. Southall et al., 2007).
Some cetaceans apparently can incur
TTS at considerably lower sound
exposures than are necessary to elicit
TTS in the beluga or bottlenose dolphin.
For baleen whales, there are no data,
direct or indirect, on levels or properties
of sound that are required to induce
TTS. The frequencies to which baleen
whales are most sensitive are assumed
to be lower than those to which
odontocetes are most sensitive, and
natural background noise levels at those
low frequencies tend to be higher. As a
result, auditory thresholds of baleen
whales within their frequency band of
best hearing are believed to be higher
(less sensitive) than are those of
odontocetes at their best frequencies
(Clark and Ellison, 2004). From this, it
is suspected that received levels causing
TTS onset may also be higher in baleen
whales than those of odontocetes
(Southall et al., 2007).
In pinnipeds, researchers have not
measured TTS thresholds associated
with exposure to brief pulses (single or
multiple) of underwater sound. Initial
evidence from more prolonged (nonpulse) exposures suggested that some
pinnipeds (harbor seals in particular)
incur TTS at somewhat lower received
levels than do small odontocetes
exposed for similar durations (Kastak et
al., 1999, 2005; Ketten et al., 2001). The
TTS threshold for pulsed sounds has
been indirectly extimated as being an
SEL of approximately 171 dB re 1 mPa2·s
(Southall et al., 2007) which would be
equivalent to a single pulse with a
received level of approximately 181 to
186 dB re 1 mPa (rms), or a series of
pulses for which the highest rms values
are a few dB lower. Corresponding
values for California sea lions and
northern elephant seals (Mirounga
angustirostris) are likely to be higher
(Kastak et al., 2005).
Permanent Threshold Shift—When
PTS occurs, there is physical damage to
the sound receptors in the ear. In severe
cases, there can be total or partial
deafness, whereas in other cases, the
animal has an impaired ability to hear
sounds in specific frequency ranges
(Kryter, 1985). There is no specific
evidence that exposure to pulses of
airgun sound can cause PTS in any
marine mammal, even with large arrays
of airguns. However, given the
possibility that mammals close to an
airgun array might incur at least mild
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TTS, there has been further speculation
about the possibility that some
individuals occurring very close to
airguns might incur PTS (e.g.,
Richardson et al., 1995, p. 372ff;
Gedamke et al., 2008). Single or
occasional occurrences of mild TTS are
not indicative of permanent auditory
damage, but repeated or (in some cases)
single exposures to a level well above
that causing TTS onset might elicit PTS.
Relationships between TTS and PTS
thresholds have not been studied in
marine mammals but are assumed to be
similar to those in humans and other
terrestrial mammals (Southall et al.,
2007). PTS might occur at a received
sound level at least several dBs above
that inducing mild TTS if the animal
were exposed to strong sound pulses
with rapid rise times. Based on data
from terrestrial mammals, a
precautionary assumption is that the
PTS threshold for impulse sounds (such
as airgun pulses as received close to the
source) is at least 6 dB higher than the
TTS threshold on a peak-pressure basis,
and probably greater than 6 dB (Southall
et al., 2007).
Given the higher level of sound
necessary to cause PTS as compared
with TTS, it is considerably less likely
that PTS would occur. Baleen whales
generally avoid the immediate area
around operating seismic vessels, as do
some other marine mammals.
Stranding and Mortality—When a
living or dead marine mammal swims or
floats onto shore and becomes
‘‘beached’’ or incapable of returning to
sea, the event is termed a ‘‘stranding’’
(Geraci et al., 1999; Perrin and Geraci,
2002; Geraci and Lounsbury, 2005;
NMFS, 2007). The legal definition for a
stranding under the MMPA is that ‘‘(A)
a marine mammal is dead and is (i) on
a beach or shore of the United States; or
(ii) in waters under the jurisdiction of
the United States (including any
navigable waters); or (B) a marine
mammal is alive and is (i) on a beach
or shore of the United States and is
unable to return to the water; (ii) on a
beach or shore of the United States and,
although able to return to the water is
in need of apparent medical attention;
or (iii) in the waters under the
jurisdiction of the United States
(including any navigable waters), but is
unable to return to its natural habitat
under its own power or without
assistance.’’
Marine mammals are known to strand
for a variety of reasons, such as
infectious agents, biotoxicosis,
starvation, fishery interaction, ship
strike, unusual oceanographic or
weather events, sound exposure, or
combinations of these stressors
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sustained concurrently or in series.
However, the cause or causes of most
strandings are unknown (Geraci et al.,
1976; Eaton, 1979; Odell et al., 1980;
Best, 1982). Numerous studies suggest
that the physiology, behavior, habitat
relationships, age, or condition of
cetaceans may cause them to strand or
might pre-dispose them to strand when
exposed to another phenomenon. These
suggestions are consistent with the
conclusions of numerous other studies
that have demonstrated that
combinations of dissimilar stressors
commonly combine to kill an animal or
dramatically reduce its fitness, even
though one exposure without the other
does not produce the same result
(Chroussos, 2000; Creel, 2005; DeVries
et al., 2003; Fair and Becker, 2000; Foley
et al., 2001; Moberg, 2000; Relyea,
2005a, 2005b; Romero, 2004; Sih et al.,
2004).
Strandings Associated With Military
Active Sonar—Several sources have
published lists of mass stranding events
of cetaceans in an attempt to identify
relationships between those stranding
events and military active sonar
(Hildebrand, 2004; IWC, 2005; Taylor et
al., 2004). For example, based on a
review of stranding records between
1960 and 1995, the International
Whaling Commission (2005) identified
ten mass stranding events and
concluded that, out of eight stranding
events reported from the mid-1980s to
the summer of 2003, seven had been
coincident with the use of midfrequency active sonar and most
involved beaked whales.
Over the past 12 years, there have
been five stranding events coincident
with military mid-frequency active
sonar use in which exposure to sonar is
believed to have been a contributing
factor to strandings: Greece (1996); the
Bahamas (2000); Madeira (2000); Canary
Islands (2002); and Spain (2006). Refer
to Cox et al. (2006) for a summary of
common features shared by the
strandings events in Greece (1996),
Bahamas (2000), Madeira (2000), and
Canary Islands (2002); and Fernandez et
al., (2005) for an additional summary of
the Canary Islands 2002 stranding event.
Potential for Stranding From Seismic
Surveys—Marine mammals close to
underwater detonations of high
explosives can be killed or severely
injured, and the auditory organs are
especially susceptible to injury (Ketten
et al., 1993; Ketten, 1995). However,
explosives are no longer used in marine
waters for commercial seismic surveys
or (with rare exceptions) for seismic
research. These methods have been
replaced entirely by airguns or related
non-explosive pulse generators. Airgun
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pulses are less energetic and have
slower rise times, and there is no
specific evidence that they can cause
serious injury, death, or stranding even
in the case of large airgun arrays.
However, the association of strandings
of beaked whales with naval exercises
involving mid-frequency active sonar
(non-pulse sound) and, in one case, the
co-occurrence of an L–DEO seismic
survey (Malakoff, 2002; Cox et al.,
2006), has raised the possibility that
beaked whales exposed to strong
‘‘pulsed’’ sounds could also be
susceptible to injury and/or behavioral
reactions that can lead to stranding (e.g.,
Hildebrand, 2005; Southall et al., 2007).
Specific sound-related processes that
lead to strandings and mortality are not
well documented, but may include:
(1) Swimming in avoidance of a
sound into shallow water;
(2) A change in behavior (such as a
change in diving behavior) that might
contribute to tissue damage, gas bubble
formation, hypoxia, cardiac arrhythmia,
hypertensive hemorrhage or other forms
of trauma;
(3) A physiological change such as a
vestibular response leading to a
behavioral change or stress-induced
hemorrhagic diathesis, leading in turn
to tissue damage; and
(4) Tissue damage directly from sound
exposure, such as through acousticallymediated bubble formation and growth
or acoustic resonance of tissues.
Some of these mechanisms are
unlikely to apply in the case of impulse
sounds. However, there are indications
that gas-bubble disease (analogous to
‘‘the bends’’), induced in supersaturated
tissue by a behavioral response to
acoustic exposure, could be a pathologic
mechanism for the strandings and
mortality of some deep-diving cetaceans
exposed to sonar. The evidence for this
remains circumstantial and associated
with exposure to naval mid-frequency
sonar, not seismic surveys (Cox et al.,
2006; Southall et al., 2007).
Seismic pulses and mid-frequency
sonar signals are quite different, and
some mechanisms by which sonar
sounds have been hypothesized to affect
beaked whales are unlikely to apply to
airgun pulses. Sounds produced by
airgun arrays are broadband impulses
with most of the energy below one kHz.
Typical military mid-frequency sonar
emits non-impulse sounds at
frequencies of 2 to 10 kHz, generally
with a relatively narrow bandwidth at
any one time. A further difference
between seismic surveys and naval
exercises is that naval exercises can
involve sound sources on more than one
vessel. Thus, it is not appropriate to
expect that the same to marine
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mammals will result from military sonar
and seismic surveys. However, evidence
that sonar signals can, in special
circumstances, lead (at least indirectly)
to physical damage and mortality (e.g.,
Balcomb and Claridge, 2001; NOAA and
USN, 2001; Jepson et al., 2003;
´
Fernandez et al., 2004, 2005;
Hildebrand 2005; Cox et al., 2006)
suggests that caution is warranted when
dealing with exposure of marine
mammals to any high-intensity sound.
There is no conclusive evidence of
cetacean strandings or deaths at sea as
a result of exposure to seismic surveys,
but a few cases of strandings in the
general area where a seismic survey was
ongoing have led to speculation
concerning a possible link between
seismic surveys and strandings.
Suggestions that there was a link
between seismic surveys and strandings
of humpback whales in Brazil (Engel et
al., 2004) were not well founded (IAGC,
2004; IWC, 2007). In September 2002,
there was a stranding of two Cuvier’s
beaked whales in the Gulf of California,
Mexico, when the L–DEO vessel R/V
Maurice Ewing was operating a 20
airgun (8,490 in3) array in the general
area. The link between the stranding
and the seismic surveys was
inconclusive and not based on any
physical evidence (Hogarth, 2002;
Yoder, 2002). Nonetheless, the Gulf of
California incident plus the beaked
whale strandings near naval exercises
involving use of mid-frequency sonar
suggests a need for caution in
conducting seismic surveys in areas
occupied by beaked whales until more
is known about effects of seismic
surveys on those species (Hildebrand,
2005). No injuries of beaked whales are
anticipated during the proposed study
because of:
(1) The high likelihood that any
beaked whales nearby would avoid the
approaching vessel before being
exposed to high sound levels, and
(2) Differences between the sound
sources operated by L–DEO and those
involved in the naval exercises
associated with strandings.
Non-auditory Physiological Effects—
Non-auditory physiological effects or
injuries that theoretically might occur in
marine mammals exposed to strong
underwater sound include stress,
neurological effects, bubble formation,
resonance, and other types of organ or
tissue damage (Cox et al., 2006; Southall
et al., 2007). Studies examining such
effects are limited. However, resonance
effects (Gentry, 2002) and direct noiseinduced bubble formations (Crum et al.,
2005) are implausible in the case of
exposure to an impulsive broadband
source like an airgun array. If seismic
PO 00000
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Sfmt 4703
479
surveys disrupt diving patterns of deepdiving species, this might perhaps result
in bubble formation and a form of the
bends, as speculated to occur in beaked
whales exposed to sonar. However,
there is no specific evidence of this
upon exposure to airgun pulses.
In general, very little is known about
the potential for seismic survey sounds
(or other types of strong underwater
sounds) to cause non-auditory physical
effects in marine mammals. Such
effects, if they occur at all, would
presumably be limited to short distances
and to activities that extend over a
prolonged period. The available data do
not allow identification of a specific
exposure level above which nonauditory effects can be expected
(Southall et al., 2007), or any
meaningful quantitative predictions of
the numbers (if any) of marine mammals
that might be affected in those ways.
Marine mammals that show behavioral
avoidance of seismic vessels, including
most baleen whales, some odontocetes,
and some pinnipeds, are especially
unlikely to incur non-auditory physical
effects.
Potential Effects of Other Acoustic
Devices and Sources
Multibeam Echosounder
NSF and ASC will operate the Simrad
EM120 multibeam echosounder from
the source vessel during the planned
study. Sounds from the multibeam
echosounder are very short pulses,
occurring for 15 ms, depending on water
depth. Most of the energy in the sound
pulses emitted by the multibeam
echosounder is at frequencies near 12
kHz, and the maximum source level is
242 dB re 1 mPa (rms). The beam is
narrow (1 to 2°) in fore-aft extent and
wide (150°) in the cross-track extent.
Each ping consists of nine (in water
greater than 1,000 m deep) consecutive
successive fan-shaped transmissions
(segments) at different cross-track
angles. Any given mammal at depth
near the trackline would be in the main
beam for only one or two of the nine
segments. Also, marine mammals that
encounter the Simrad EM120 are
unlikely to be subjected to repeated
pulses because of the narrow fore-aft
width of the beam and will receive only
limited amounts of pulse energy
because of the short pulses. Animals
close to the ship (where the beam is
narrowest) are especially unlikely to be
ensonified for more than one 15 ms
pulse (or two pulses if in the overlap
area). Similarly, Kremser et al. (2005)
noted that the probability of a cetacean
swimming through the area of exposure
when a multibeam echosounder emits a
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pulse is small. The animal would have
to pass the transducer at close range and
be swimming at speeds similar to the
vessel in order to receive the multiple
pulses that might result in sufficient
exposure to cause TTS.
Navy sonars that have been linked to
avoidance reactions and stranding of
cetaceans: (1) Generally have longer
pulse duration than the Simrad EM120;
and (2) are often directed close to
horizontally, as well as omnidirectional,
versus more downward and narrowly
for the multibeam echosounder. The
area of possible influence of the
multibeam echosounder is much
smaller—a narrow band below the
source vessel. Also, the duration of
exposure for a given marine mammal
can be much longer for naval sonar.
During NSF and ASC’s operations, the
individual pulses will be very short, and
a given mammal would not receive
many of the downward-directed pulses
as the vessel passes by. Possible effects
of a multibeam echosounder on marine
mammals are described below.
Masking—Marine mammal
communications will not be masked
appreciably by the multibeam
echosounder signals given the low duty
cycle of the echosounder and the brief
period when an individual mammal is
likely to be within its beam.
Furthermore, in the case of baleen
whales, the multibeam echosounder
signals (12 kHz) do not overlap with the
predominant frequencies in the calls,
which would avoid any significant
masking.
Behavioral Responses—Behavioral
reactions of free-ranging marine
mammals to sonars, echosounders, and
other sound sources appear to vary by
species and circumstance. Observed
reactions have included silencing and
dispersal by sperm whales (Watkins et
al., 1985), increased vocalizations and
no dispersal by pilot whales (Rendell
and Gordon, 1999), and the previouslymentioned beachings by beaked whales.
During exposure to a 21 to 25 kHz
‘‘whale-finding’’ sonar with a source
level of 215 dB re 1 mPa, gray whales
reacted by orienting slightly away from
the source and being deflected from
their course by approximately 200 m
(656.2 ft) (Frankel, 2005). When a 38
kHz echosounder and a 150 kHz
acoustic Doppler current profiler were
transmitting during studies in the
Eastern Tropical Pacific, baleen whales
showed no significant responses, while
spotted and spinner dolphins were
detected slightly more often and beaked
whales less often during visual surveys
(Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a
beluga whale exhibited changes in
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behavior when exposed to 1 second
tonal signals at frequencies similar to
those that will be emitted by the
multibeam echosounder used by NSF
and ASC, and to shorter broadband
pulsed signals. Behavioral changes
typically involved what appeared to be
deliberate attempts to avoid the sound
exposure (Schlundt et al., 2000;
Finneran et al., 2002; Finneran and
Schlundt, 2004). The relevance of those
data to free-ranging odontocetes is
uncertain, and in any case, the test
sounds were quite different in duration
as compared with those from a
multibeam echosounder.
Hearing Impairment and Other
Physical Effects—Given several
stranding events that have been
associated with the operation of naval
sonar in specific circumstances, there is
concern that mid-frequency sonar
sounds can cause serious impacts to
marine mammals (see above). However,
the multibeam echosounder proposed
for use by NSF and ASC is quite
different than sonar used for Navy
operations. Pulse duration of the
multibeam echosounder is very short
relative to the naval sonar. Also, at any
given location, an individual marine
mammal would be in the beam of the
multibeam echosounder for much less
time given the generally downward
orientation of the beam and its narrow
fore-aft beamwidth; Navy sonar often
uses near-horizontally-directed sound.
Those factors would all reduce the
sound energy received from the
multibeam echosounder rather
drastically relative to that from naval
sonar.
NMFS believes that the brief exposure
of marine mammals to one pulse, or
small numbers of signals, from the
multi-beam echosounder in this
particular case is not likely to result in
the harassment of marine mammals.
Single-Beam Echosounder
NSF and ASC will operate the
Knudsen 3260 and Bathy 2000 singlebeam echosounders from the source
vessel during the planned study.
Sounds from the single-beam
echosounder are very short pulses,
depending on water depth. Most of the
energy in the sound pulses emitted by
the singlebeam echosounder is at
frequencies near 12 kHz for bottomtracking purposes or at 3.5 kHz in the
sub-bottom profiling mode. The sonar
emits energy in a 30° beam from the
bottom of the ship. Marine mammals
that encounter the Simrad EM120 are
unlikely to be subjected to repeated
pulses because of the narrow fore–aft
width of the beam and will receive only
limited amounts of pulse energy
PO 00000
Frm 00018
Fmt 4701
Sfmt 4703
because of the short pulses. Animals
close to the ship (where the beam is
narrowest) are especially unlikely to be
ensonified for more than one 15 ms
pulse (or two pulses if in the overlap
area). Similarly, Kremser et al. (2005)
noted that the probability of a cetacean
swimming through the area of exposure
when a multibeam echosounder emits a
pulse is small. The animal would have
to pass the transducer at close range and
be swimming at speeds similar to the
vessel in order to receive the multiple
pulses that might result in sufficient
exposure to cause TTS.
Navy sonars that have been linked to
avoidance reactions and stranding of
cetaceans: (1) Generally have longer
pulse duration than the Simrad EM120;
and (2) are often directed close to
horizontally versus more downward for
the echosounder. The area of possible
influence of the single-beam
echosounder is much smaller—a narrow
band below the source vessel. Also, the
duration of exposure for a given marine
mammal can be much longer for naval
sonar. During NSF and ASC’s
operations, the individual pulses will be
very short, and a given mammal would
not receive many of the downwarddirected pulses as the vessel passes by.
Possible effects of a single-beam
echosounder on marine mammals are
described below.
Masking—Marine mammal
communications will not be masked
appreciably by the single-beam
echosounder signals given the low duty
cycle of the echosounder and the brief
period when an individual mammal is
likely to be within its beam.
Furthermore, in the case of baleen
whales, the single-beam echosounder
signals (12 or 3.5 kHz) do not overlap
with the predominant frequencies in the
calls, which would avoid any significant
masking.
Behavioral Responses—Behavioral
reactions of free-ranging marine
mammals to sonars, echosounders, and
other sound sources appear to vary by
species and circumstance. Observed
reactions have included silencing and
dispersal by sperm whales (Watkins et
al., 1985), increased vocalizations and
no dispersal by pilot whales (Rendell
and Gordon, 1999), and the previouslymentioned beachings by beaked whales.
During exposure to a 21 to 25 kHz
‘‘whale-finding’’ sonar with a source
level of 215 dB re 1 mPa, gray whales
reacted by orienting slightly away from
the source and being deflected from
their course by approximately 200 m
(656.2 ft) (Frankel, 2005). When a 38
kHz echosounder and a 150 kHz ADCP
were transmitting during studies in the
Eastern Tropical Pacific, baleen whales
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showed no significant responses, while
spotted and spinner dolphins were
detected slightly more often and beaked
whales less often during visual surveys
(Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a
beluga whale exhibited changes in
behavior when exposed to 1 second
tonal signals at frequencies similar to
those that will be emitted by the singlebeam echosounder used by NSF and
ASC, and to shorter broadband pulsed
signals. Behavioral changes typically
involved what appeared to be deliberate
attempts to avoid the sound exposure
(Schlundt et al., 2000; Finneran et al.,
2002; Finneran and Schlundt, 2004).
The relevance of those data to freeranging odontocetes is uncertain, and in
any case, the test sounds were quite
different in duration as compared with
those from a single-beam echosounder.
Hearing Impairment and Other
Physical Effects—Given recent stranding
events that have been associated with
the operation of naval sonar, there is
concern that mid-frequency sonar
sounds can cause serious impacts to
marine mammals (see above). However,
the single-beam echosounder proposed
for use by NSF and ASC is quite
different than sonar used for Navy
operations. Pulse duration of the singlebeam echosounder is very short relative
to the naval sonar. Also, at any given
location, an individual marine mammal
would be in the beam of the single-beam
echosounder for much less time given
the generally downward orientation of
the beam and its narrow fore-aft
beamwidth; Navy sonar often uses nearhorizontally-directed sound. Those
factors would all reduce the sound
energy received from the single-beam
echosounder rather drastically relative
to that from naval sonar.
NMFS believes that the brief exposure
of marine mammals to one pulse, or
small numbers of signals, from the
single-beam echosounder in this
particular case is not likely to result in
the harassment of marine mammals.
Acoustic Doppler Current Profilers
NSF and ASC will operate the ADCP
Teledyne RDI VM–150 and ADCP Ocean
Surveyor OS–38 from the source vessel
during the planned study. Most of the
energy in the sound pulses emitted by
the ADCPs operate at frequencies near
150 kHz, and the maximum source level
is 223.6 dB re 1 mPa (rms). Sound energy
from the ADCP is emitted as a 30°
conically-shaped beam. Marine
mammals that encounter the ADCPs are
unlikely to be subjected to repeated
pulses because of the narrow fore–aft
width of the beam and will receive only
limited amounts of pulse energy
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because of the short pulses. Animals
close to the ship (where the beam is
narrowest) are especially unlikely to be
ensonified for more than one 15 ms
pulse (or two pulses if in the overlap
area). Similarly, Kremser et al. (2005)
noted that the probability of a cetacean
swimming through the area of exposure
when the ADCPs emits a pulse is small.
The animal would have to pass the
transducer at close range and be
swimming at speeds similar to the
vessel in order to receive the multiple
pulses that might result in sufficient
exposure to cause TTS.
Navy sonars that have been linked to
avoidance reactions and stranding of
cetaceans: (1) Generally have longer
pulse duration than the ADCPs; and (2)
are often directed close to horizontally
versus more downward for the ADCPs.
The area of possible influence of the
multibeam echosounder is much
smaller—a narrow band below the
source vessel. Also, the duration of
exposure for a given marine mammal
can be much longer for naval sonar.
During NSF and ASC’s operations, the
individual pulses will be very short, and
a given mammal would not receive
many of the downward-directed pulses
as the vessel passes by. Possible effects
of the ADCPs on marine mammals are
described below.
Masking—Marine mammal
communications will not be masked
appreciably by the ADCP signals given
the low duty cycle of the ADCPs and the
brief period when an individual
mammal is likely to be within its beam.
Furthermore, in the case of baleen
whales, the ADCP signals (150 kHz) do
not overlap with the predominant
frequencies in the calls, which would
avoid any significant masking.
Behavioral Responses—Behavioral
reactions of free-ranging marine
mammals to sonars, echosounders, and
other sound sources appear to vary by
species and circumstance. Observed
reactions have included silencing and
dispersal by sperm whales (Watkins et
al., 1985), increased vocalizations and
no dispersal by pilot whales (Rendell
and Gordon, 1999), and the previouslymentioned beachings by beaked whales.
During exposure to a 21 to 25 kHz
‘‘whale-finding’’ sonar with a source
level of 215 dB re 1 mPa, gray whales
reacted by orienting slightly away from
the source and being deflected from
their course by approximately 200 m
(656.2 ft) (Frankel, 2005). When a 38
kHz echosounder and a 150 kHz ADCP
were transmitting during studies in the
Eastern Tropical Pacific, baleen whales
showed no significant responses, while
spotted and spinner dolphins were
detected slightly more often and beaked
PO 00000
Frm 00019
Fmt 4701
Sfmt 4703
481
whales less often during visual surveys
(Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a
beluga whale exhibited changes in
behavior when exposed to 1 second
tonal signals at frequencies similar to
those that will be emitted by the
multibeam echosounder used by NSF
and ASC, and to shorter broadband
pulsed signals. Behavioral changes
typically involved what appeared to be
deliberate attempts to avoid the sound
exposure (Schlundt et al., 2000;
Finneran et al., 2002; Finneran and
Schlundt, 2004). The relevance of those
data to free-ranging odontocetes is
uncertain, and in any case, the test
sounds were quite different in duration
as compared with those from a
multibeam echosounder.
Hearing Impairment and Other
Physical Effects—Given recent stranding
events that have been associated with
the operation of naval sonar, there is
concern that mid-frequency sonar
sounds can cause serious impacts to
marine mammals (see above). However,
the multibeam echosounder proposed
for use by NSF and ASC is quite
different than sonar used for Navy
operations. Pulse duration of the ADCP
is very short relative to the naval sonar.
Also, at any given location, an
individual marine mammal would be in
the beam of the multibeam echosounder
for much less time given the generally
downward orientation of the beam and
its narrow fore-aft beamwidth; Navy
sonar often uses near-horizontallydirected sound. Those factors would all
reduce the sound energy received from
the multibeam echosounder rather
drastically relative to that from naval
sonar.
NMFS believes that the brief exposure
of marine mammals to one pulse, or
small numbers of signals, from the
multi-beam echosounder in this
particular case is not likely to result in
the harassment of marine mammals.
Acoustic Locator
NSF and ASC will operate the
acoustic locator from the source vessel
during the planned study during
sampling. Sounds from the locator are
very short pulses, occurring for 5 ms.
Most of the energy in the sound pulses
emitted by the acoustic locator is at
frequencies near 12 kHz, and the
maximum source level is 162 dB re 1
mPa (rms). Animals close to the ship
(where the beam is narrowest) are
especially unlikely to be ensonified for
more than one 5 ms pulse (or two pulses
if in the overlap area). Similarly,
Kremser et al. (2005) noted that the
probability of a cetacean swimming
through the area of exposure when a
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multibeam echosounder emits a pulse is
small. The animal would have to pass
the transducer at close range and be
swimming at speeds similar to the
vessel in order to receive the multiple
pulses that might result in sufficient
exposure to cause TTS.
Masking—Marine mammal
communications will not be masked
appreciably by the acoustic locator
signals given the low duty cycle and the
low source level. Furthermore, in the
case of baleen whales, the acoustic
locator signals (12 kHz) do not overlap
with the predominant frequencies in the
calls, which would avoid any significant
masking.
Behavioral Responses—Behavioral
reactions of free-ranging marine
mammals to sonars, echosounders, and
other sound sources appear to vary by
species and circumstance. Observed
reactions have included silencing and
dispersal by sperm whales (Watkins et
al., 1985), increased vocalizations and
no dispersal by pilot whales (Rendell
and Gordon, 1999), and the previouslymentioned beachings by beaked whales.
During exposure to a 21 to 25 kHz
‘‘whale-finding’’ sonar with a source
level of 215 dB re 1 mPa, gray whales
reacted by orienting slightly away from
the source and being deflected from
their course by approximately 200 m
(656.2 ft) (Frankel, 2005). When a 38
kHz echosounder and a 150 kHz ADCP
were transmitting during studies in the
Eastern Tropical Pacific, baleen whales
showed no significant responses, while
spotted and spinner dolphins were
detected slightly more often and beaked
whales less often during visual surveys
(Gerrodette and Pettis, 2005).
NMFS believes that the brief exposure
of marine mammals to one pulse, or
small numbers of signals, from the
acoustic locator is not likely to result in
the harassment of marine mammals.
Core and Dredge Sampling
During coring and dredging, the noise
created by the mechanical action of the
devices on the seafloor is expected to be
perceived by nearby fish and other
marine organisms and deter them from
swimming toward the source. Coring
and dredging activities would be highly
localized and short-term in duration and
would not be expected to significantly
interfere with marine mammal behavior.
The potential direct effects include
temporary localized disturbance or
displacement from associated sounds
and/or physical movement/actions of
the operations. Additionally, the
potential indirect effects may consist of
very localized and transitory/short-term
disturbance of bottom habitat and
associated prey in shallow-water areas
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as a result of coring, dredging, and
sediment sampling (NSF/USGS PEIS,
2011). NMFS believes that the brief
exposure of marine mammals to noise
created from the mechanical action of
the devices for core and dredge
sampling is not likely to result in the
harassment of marine mammals.
Vessel Movement and Collisions
Vessel movement in the vicinity of
marine mammals has the potential to
result in either a behavioral response or
a direct physical interaction. Both
scenarios are discussed below in this
section.
Behavioral Responses to Vessel
Movement—There are limited data
concerning marine mammal behavioral
responses to vessel traffic and vessel
noise, and a lack of consensus among
scientists with respect to what these
responses mean or whether they result
in short-term or long-term adverse
effects. In those cases where there is a
busy shipping lane or where there is a
large amount of vessel traffic, marine
mammals (especially low frequency
specialists) may experience acoustic
masking (Hildebrand, 2005) if they are
present in the area (e.g., killer whales in
Puget Sound; Foote et al., 2004; Holt et
al., 2008). In cases where vessels
actively approach marine mammals
(e.g., whale watching or dolphin
watching boats), scientists have
documented that animals exhibit altered
behavior such as increased swimming
speed, erratic movement, and active
avoidance behavior (Bursk, 1983;
Acevedo, 1991; Baker and MacGibbon,
1991; Trites and Bain, 2000; Williams et
al., 2002; Constantine et al., 2003),
reduced blow interval (Ritcher et al.,
2003), disruption of normal social
behaviors (Lusseau, 2003, 2006), and the
shift of behavioral activities which may
increase energetic costs (Constantine et
al., 2003, 2004). A detailed review of
marine mammal reactions to ships and
boats is available in Richardson et al.,
(1995). For each of the marine mammal
taxonomy groups, Richardson et al.,
(1995) provides the following
assessment regarding reactions to vessel
traffic:
Toothed whales—‘‘In summary,
toothed whales sometimes show no
avoidance reaction to vessels, or even
approach them. However, avoidance can
occur, especially in response to vessels
of types used to chase or hunt the
animals. This may cause temporary
displacement, but we know of no clear
evidence that toothed whales have
abandoned significant parts of their
range because of vessel traffic.’’
Baleen whales—‘‘When baleen whales
receive low-level sounds from distant or
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Fmt 4701
Sfmt 4703
stationary vessels, the sounds often
seem to be ignored. Some whales
approach the sources of these sounds.
When vessels approach whales slowly
and non-aggressively, whales often
exhibit slow and inconspicuous
avoidance maneuvers. In response to
strong or rapidly changing vessel noise,
baleen whales often interrupt their
normal behavior and swim rapidly
away. Avoidance is especially strong
when a boat heads directly toward the
whale.’’
Behavioral responses to stimuli are
complex and influenced to varying
degrees by a number of factors, such as
species, behavioral contexts,
geographical regions, source
characteristics (moving or stationary,
speed, direction, etc.), prior experience
of the animal and physical status of the
animal. For example, studies have
shown that beluga whales’ reaction
varied when exposed to vessel noise
and traffic. In some cases, beluga whales
exhibited rapid swimming from icebreaking vessels up to 80 km (43.2 nmi)
away and showed changes in surfacing,
breathing, diving, and group
composition in the Canadian high
Arctic where vessel traffic is rare (Finley
et al., 1990). In other cases, beluga
whales were more tolerant of vessels,
but responded differentially to certain
vessels and operating characteristics by
reducing their calling rates (especially
older animals) in the St. Lawrence River
where vessel traffic is common (Blane
and Jaakson, 1994). In Bristol Bay,
Alaska, beluga whales continued to feed
when surrounded by fishing vessels and
resisted dispersal even when
purposefully harassed (Fish and Vania,
1971).
In reviewing more than 25 years of
whale observation data, Watkins (1986)
concluded that whale reactions to vessel
traffic were ‘‘modified by their previous
experience and current activity:
habituation often occurred rapidly,
attention to other stimuli or
preoccupation with other activities
sometimes overcame their interest or
wariness of stimuli.’’ Watkins noticed
that over the years of exposure to ships
in the Cape Cod area, minke whales
changed from frequent positive interest
(e.g., approaching vessels) to generally
uninterested reactions; fin whales
changed from mostly negative (e.g.,
avoidance) to uninterested reactions; fin
whales changed from mostly negative
(e.g., avoidance) to uninterested
reactions; right whales apparently
continued the same variety of responses
(negative, uninterested, and positive
responses) with little change; and
humpbacks dramatically changed from
mixed responses that were often
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negative to reactions that were often
strongly positive. Watkins (1986)
summarized that ‘‘whales near shore,
even in regions with low vessel traffic,
generally have become less wary of
boats and their noises, and they have
appeared to be less easily disturbed than
previously. In particular locations with
intense shipping and repeated
approaches by boats (such as the whalewatching areas of Stellwagen Bank),
more and more whales had positive
reactions to familiar vessels, and they
also occasionally approached other
boats and yachts in the same ways.’’
Although the radiated sound from the
Palmer will be audible to marine
mammals over a large distance, it is
unlikely that marine mammals will
respond behaviorally (in a manner that
NMFS would consider harassment
under the MMPA) to low-level distant
shipping noise as the animals in the
area are likely to be habituated to such
noises (Nowacek et al., 2004). In light of
these facts, NMFS does not expect the
Palmer’s movements to result in Level B
harassment.
Vessel Strike—Ship strikes of
cetaceans can cause major wounds,
which may lead to the death of the
animal. An animal at the surface could
be struck directly by a vessel, a
surfacing animal could hit the bottom of
a vessel, or an animal just below the
surface could be cut by a vessel’s
propeller. The severity of injuries
typically depends on the size and speed
of the vessel (Knowlton and Kraus,
2001; Laist et al., 2001; Vanderlaan and
Taggart, 2007).
The most vulnerable marine mammals
are those that spend extended periods of
time at the surface in order to restore
oxygen levels within their tissues after
deep dives (e.g., the sperm whale). In
addition, some baleen whales, such as
the North Atlantic right whale, seem
generally unresponsive to vessel sound,
making them more susceptible to vessel
collisions (Nowacek et al., 2004). These
species are primarily large, slow moving
whales. Smaller marine mammals (e.g.,
bottlenose dolphin) move quickly
through the water column and are often
seen riding the bow wave of large ships.
Marine mammal responses to vessels
may include avoidance and changes in
dive pattern (NRC, 2003).
An examination of all known ship
strikes from all shipping sources
(civilian and military) indicates vessel
speed is a principal factor in whether a
vessel strike results in death (Knowlton
and Kraus, 2001; Laist et al., 2001;
Jensen and Silber, 2003; Vanderlaan and
Taggart, 2007). In assessing records in
which vessel speed was known, Laist et
al. (2001) found a direct relationship
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between the occurrence of a whale
strike and the speed of the vessel
involved in the collision. The authors
concluded that most deaths occurred
when a vessel was traveling in excess of
13 kts (24.1 km/hr, 14.9 mph).
NSF and ASC’s proposed operation of
one source vessel for the proposed lowenergy seismic survey is relatively small
in scale compared to the number of
commercial ships transiting at higher
speeds in the same areas on an annual
basis. The probability of vessel and
marine mammal interactions occurring
during the proposed low-energy seismic
survey is unlikely due to the Palmer’s
slow operational speed, which is
typically 5 kts. Outside of seismic
operations, the Palmer’s cruising speed
would be approximately 10.1 to 14.5
kts, which is generally below the speed
at which studies have noted reported
increases of marine mammal injury or
death (Laist et al., 2001).
As a final point, the Palmer has a
number of other advantages for avoiding
ship strikes as compared to most
commercial merchant vessels, including
the following: the Palmer’s bridge and
aloft observation tower offers good
visibility to visually monitor for marine
mammal presence; PSOs posted during
operations scan the ocean for marine
mammals and must report visual alerts
of marine mammal presence to crew;
and the PSOs receive extensive training
that covers the fundamentals of visual
observing for marine mammals and
information about marine mammals and
their identification at sea.
Entanglement
Entanglement can occur if wildlife
becomes immobilized in survey lines,
cables, nets, or other equipment that is
moving through the water column. The
proposed low-energy seismic survey
would require towing approximately a
single 100 m cable streamer. This large
of an array carries the risk of
entanglement for marine mammals.
Wildlife, especially slow moving
individuals, such as large whales, have
a low probability of becoming entangled
due to slow speed of the survey vessel
and onboard monitoring efforts. In May
2011, there was one recorded
entanglement of an olive ridley sea
turtle (Lepidochelys olivacea) in the R/
V Marcus G. Langseth’s barovanes after
the conclusion of a seismic survey off
Costa Rica. There have been cases of
baleen whales, mostly gray whales
(Heyning, 1990), becoming entangled in
fishing lines. The probability for
entanglement of marine mammals is
considered not significant because of
the vessel speed and the monitoring
efforts onboard the survey vessel.
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483
Icebreaking Activities
Icebreakers produce more noise while
breaking ice than ships of comparable
size due, primarily, to the sounds of
propeller cavitating (Richardson et al.,
1995). Multi-year ice, which is expected
to be encountered in the proposed
survey area. Icebreakers commonly back
and ram into heavy ice until losing
momentum to make way. The highest
noise levels usually occur while backing
full astern in preparation to ram forward
through the ice. Overall the noise
generated by an icebreaker pushing ice
was 10 to 15 dB greater than the noise
produced by the ship underway in open
water (Richardson et al., 1995). In
general, the Antarctic and Southern
Ocean is a noisy environment. Calving
and grounding icebergs as well as the
break-up of ice sheets, can produce a
large amount of underwater noise. Little
information is available about the
increased sound levels due to
icebreaking.
Cetaceans—Few studies have been
conducted to evaluate the potential
interference of icebreaking noise with
marine mammal vocalizations. Erbe and
Farmer (1998) measured masked hearing
thresholds of a captive beluga whale.
They reported that the recording of a
CCG ship, Henry Larsen, ramming ice in
the Beaufort Sea, masked recordings of
beluga vocalizations at a noise to signal
pressure ratio of 18 dB, when the noise
pressure level was eight times as high as
the call pressure. Erbe and Farmer
(2000) also predicted when icebreaker
noise would affect beluga whales
through software that combined a sound
propagation model and beluga whale
impact threshold models. They again
used the data from the recording of the
Henry Larsen in the Beaufort Sea and
predicted that masking of beluga whale
vocalizations could extend between 40
and 71 km (21.6 and 38.3 nmi) near the
surface. Lesage et al. (1999) report that
beluga whales changed their call type
and call frequency when exposed to
boat noise. It is possible that the whales
adapt to the ambient noise levels and
are able to communicate despite the
sound. Given the documented reaction
of belugas to ships and icebreakers it is
highly unlikely that beluga whales
would remain in the proximity of
vessels where vocalizations would be
masked.
Beluga whales have been documented
swimming rapidly away from ships and
icebreakers in the Canadian high Arctic
when a ship approaches to within 35 to
50 km (18.9 to 27 nmi), and they may
travel up to 80 km (43.2 nmi) from the
vessel’s track (Richardson et al., 1995).
It is expected that belugas avoid
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icebreakers as soon as they detect the
ships (Cosens and Dueck, 1993).
However, the reactions of beluga whales
to ships vary greatly and some animals
may become habituated to high levels of
ambient noise (Erbe and Darmber,
2000).
There is little information about the
effects of icebreaking ships on baleen
whales. Migrating bowhead whales
appeared to avoid an area around a drill
site by greater than 25 km (13.5 mi)
where an icebreaker was working in the
Beaufort Sea. There was intensive
icebreaking daily in support of the
drilling activities (Brewer et al., 1993).
Migrating bowheads also avoided a
nearby drill site at the same time of year
where little icebreaking was being
conducted (LGL and Greeneridge, 1987).
It is unclear as to whether the drilling
activities, icebreaking operations, or the
ice itself might have been the cause for
the whale’s diversion. Bowhead whales
are not expected to occur in the
proximity of the proposed action area.
Pinnipeds—Brueggeman et al. (1992)
reported on the reactions of seals to an
icebreaker during activities at two
prospects in the Chukchi Sea. Reactions
of seals to the icebreakers varied
between the two prospects. Most (67%)
seals did not react to the icebreaker at
either prospect. Reaction at one
prospect was greatest during icebreaking
activity (running/maneuvering/jogging)
and was 0.23 km (0.12 nmi) of the vessel
and lowest for animals beyond 0.93 km
(0.5 nmi). At the second prospect
however, seal reaction was lowest
during icebreaking activity with higher
and similar levels of response during
general (non-icebreaking) vessel
operations and when the vessel was at
anchor or drifting. The frequency of seal
reaction generally declined with
increasing distance from the vessel
except during general vessel activity
where it remained consistently high to
about 0.46 km (0.25 nmi) from the
vessel before declining.
Similarly, Kanik et al. (1980) found
that ringed (Pusa hispida) and harp
seals (Pagophilus groenlandicus) often
dove into the water when an icebreaker
was breaking ice within 1 km (0.5 nmi)
of the animals. Most seals remained on
the ice when the ship was breaking ice
1 to 2 km (0.5 to 1.1 nmi) away.
The potential effects to marine
mammals described in this section of
the document do not take into
consideration the proposed monitoring
and mitigation measures described later
in this document (see the ‘‘Proposed
Mitigation’’ and ‘‘Proposed Monitoring
and Reporting’’ sections) which, as
noted are designed to effect the least
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practicable adverse impact on affected
marine mammal species and stocks.
Anticipated Effects on Marine Mammal
Habitat
The proposed seismic survey is not
anticipated to have any permanent
impact on habitats used by the marine
mammals in the proposed survey area,
including the food sources they use (i.e.
fish and invertebrates). Additionally, no
physical damage to any habitat is
anticipated as a result of conducting
airgun operations during the proposed
low-energy seismic survey. While it is
anticipated that the specified activity
may result in marine mammals avoiding
certain areas due to temporary
ensonification, this impact to habitat is
temporary and was considered in
further detail earlier in this document,
as behavioral modification. The main
impact associated with the proposed
activity will be temporarily elevated
noise levels and the associated direct
effects on marine mammals in any
particular area of the approximately
5,628 km2 proposed project area,
previously discussed in this notice.
The Palmer is designed for
continuous passage at 3 kts through ice
1 m thick. During the proposed project
the Palmer will typically encounter
first- or second-year ice while avoiding
thicker ice floes, particularly large intact
multi-year ice, whenever possible. In
addition, the vessel will follow leads
when possible while following the
survey route. As the vessel passes
through the ice, the ship causes the ice
to part and travel alongside the hull.
This ice typically returns to fill the
wake as the ship passes. The effects are
transitory (i.e., hours at most) and
localized (i.e., constrained to a relatively
narrow swath perhaps 10 m (32.1 ft) to
each side of the vessel. The Palmer’s
maximum beam is 18.3 m (60 ft).
Applying the maximum estimated
amount of icebreaking (1,000 km), to the
corridor opened by the ship, NSF and
ASC anticipate that a maximum of
approximately 18 km2 (5.3 nmi2) of ice
may be disturbed. This represents an
inconsequential amount of the total ice
present in the Southern Ocean.
Sea ice is important for pinniped life
functions such as resting, breeding, and
molting. Icebreaking activities may
damage seal breathing holes and will
also reduce the haul-out area in the
immediate vicinity of the ship’s track.
Icebreaking along a maximum of 1,000
km of trackline will alter local ice
conditions in the immediate vicinity of
the vessel. This has the potential to
temporarily lead to a reduction of
suitable seal haul-out habitat. However,
the dynamic sea-ice environment
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requires that seals be able to adapt to
changes in sea, ice, and snow
conditions, and they therefore create
new breathing holes and lairs
throughout the winter and spring
(Hammill and Smith, 1989). In addition,
seals often use open leads and cracks in
the ice to surface and breathe (Smith
and Stirling, 1975). Disturbance of the
ice will occur in a very small area
relative to the Southern Ocean ice-pack
and no significant impact on marine
mammals is anticipated by icebreaking
during the proposed low-energy seismic
survey. The next section discusses the
potential impacts of anthropogenic
sound sources on common marine
mammal prey in the proposed survey
area (i.e., fish and invertebrates).
Anticipated Effects on Fish
One reason for the adoption of airguns
as the standard energy source for marine
seismic surveys is that, unlike
explosives, they have not been
associated with large-scale fish kills.
However, existing information on the
impacts of seismic surveys on marine
fish and invertebrate populations is
limited. There are three types of
potential effects of exposure to seismic
surveys: (1) Pathological, (2)
physiological, and (3) behavioral.
Pathological effects involve lethal and
temporary or permanent sub-lethal
injury. Physiological effects involve
temporary and permanent primary and
secondary stress responses, such as
changes in levels of enzymes and
proteins. Behavioral effects refer to
temporary and (if they occur) permanent
changes in exhibited behavior (e.g.,
startle and avoidance behavior). The
three categories are interrelated in
complex ways. For example, it is
possible that certain physiological and
behavioral changes could potentially
lead to an ultimate pathological effect
on individuals (i.e., mortality).
The specific received sound levels at
which permanent adverse effects to fish
potentially could occur are little studied
and largely unknown. Furthermore, the
available information on the impacts of
seismic surveys on marine fish is from
studies of individuals or portions of a
population; there have been no studies
at the population scale. The studies of
individual fish have often been on caged
fish that were exposed to airgun pulses
in situations not representative of an
actual seismic survey. Thus, available
information provides limited insight on
possible real-world effects at the ocean
or population scale. This makes drawing
conclusions about impacts on fish
problematic because, ultimately, the
most important issues concern effects
on marine fish populations, their
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viability, and their availability to
fisheries.
Hastings and Popper (2005), Popper
(2009), and Popper and Hastings (2009a,
b) provided recent critical reviews of the
known effects of sound on fish. The
following sections provide a general
synopsis of the available information on
the effects of exposure to seismic and
other anthropogenic sound as relevant
to fish. The information comprises
results from scientific studies of varying
degrees of rigor plus some anecdotal
information. Some of the data sources
may have serious shortcomings in
methods, analysis, interpretation, and
reproducibility that must be considered
when interpreting their results (see
Hastings and Popper, 2005). Potential
adverse effects of the program’s sound
sources on marine fish are noted.
Pathological Effects—The potential
for pathological damage to hearing
structures in fish depends on the energy
level of the received sound and the
physiology and hearing capability of the
species in question. For a given sound
to result in hearing loss, the sound must
exceed, by some substantial amount, the
hearing threshold of the fish for that
sound (Popper, 2005). The
consequences of temporary or
permanent hearing loss in individual
fish on a fish population are unknown;
however, they likely depend on the
number of individuals affected and
whether critical behaviors involving
sound (e.g., predator avoidance, prey
capture, orientation and navigation,
reproduction, etc.) are adversely
affected.
Little is known about the mechanisms
and characteristics of damage to fish
that may be inflicted by exposure to
seismic survey sounds. Few data have
been presented in the peer-reviewed
scientific literature. As far as NSF, ASC,
and NMFS know, there are only two
papers with proper experimental
methods, controls, and careful
pathological investigation implicating
sounds produced by actual seismic
survey airguns in causing adverse
anatomical effects. One such study
indicated anatomical damage, and the
second indicated TTS in fish hearing.
The anatomical case is McCauley et al.
(2003), who found that exposure to
airgun sound caused observable
anatomical damage to the auditory
maculae of pink snapper (Pagrus
auratus). This damage in the ears had
not been repaired in fish sacrificed and
examined almost two months after
exposure. On the other hand, Popper et
al. (2005) documented only TTS (as
determined by auditory brainstem
response) in two of three fish species
from the Mackenzie River Delta. This
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study found that broad whitefish
(Coregonus nasus) exposed to five
airgun shots were not significantly
different from those of controls. During
both studies, the repetitive exposure to
sound was greater than would have
occurred during a typical seismic
survey. However, the substantial lowfrequency energy produced by the
airguns (less than 400 Hz in the study
by McCauley et al. [2003] and less than
approximately 200 Hz in Popper et al.
[2005]) likely did not propagate to the
fish because the water in the study areas
was very shallow (approximately nine
m in the former case and less than two
m in the latter). Water depth sets a
lower limit on the lowest sound
frequency that will propagate (the
‘‘cutoff frequency’’) at about one-quarter
wavelength (Urick, 1983; Rogers and
Cox, 1988).
Wardle et al. (2001) suggested that in
water, acute injury and death of
organisms exposed to seismic energy
depends primarily on two features of
the sound source: (1) The received peak
pressure, and (2) the time required for
the pressure to rise and decay.
Generally, as received pressure
increases, the period for the pressure to
rise and decay decreases, and the
chance of acute pathological effects
increases. According to Buchanan et al.
(2004), for the types of seismic airguns
and arrays involved with the proposed
program, the pathological (mortality)
zone for fish would be expected to be
within a few meters of the seismic
source. Numerous other studies provide
examples of no fish mortality upon
exposure to seismic sources (Falk and
Lawrence, 1973; Holliday et al., 1987;
La Bella et al., 1996; Santulli et al.,
1999; McCauley et al., 2000a, b, 2003;
Bjarti, 2002; Thomsen, 2002; Hassel et
al., 2003; Popper et al., 2005; Boeger et
al., 2006).
An experiment of the effects of a
single 700 in3 airgun was conducted in
Lake Meade, Nevada (USGS, 1999). The
data were used in an Environmental
Assessment of the effects of a marine
reflection survey of the Lake Meade
fault system by the National Park
Service (Paulson et al., 1993, in USGS,
1999). The airgun was suspended 3.5 m
(11.5 ft) above a school of threadfin shad
in Lake Meade and was fired three
successive times at a 30 second interval.
Neither surface inspection nor diver
observations of the water column and
bottom found any dead fish.
For a proposed seismic survey in
Southern California, USGS (1999)
conducted a review of the literature on
the effects of airguns on fish and
fisheries. They reported a 1991 study of
the Bay Area Fault system from the
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485
continental shelf to the Sacramento
River, using a 10 airgun (5,828 in3)
array. Brezzina and Associates were
hired by USGS to monitor the effects of
the surveys and concluded that airgun
operations were not responsible for the
death of any of the fish carcasses
observed. They also concluded that the
airgun profiling did not appear to alter
the feeding behavior of sea lions, seals,
or pelicans observed feeding during the
seismic surveys.
Some studies have reported, some
equivocally, that mortality of fish, fish
eggs, or larvae can occur close to
seismic sources (Kostyuchenko, 1973;
Dalen and Knutsen, 1986; Booman et
al., 1996; Dalen et al., 1996). Some of
the reports claimed seismic effects from
treatments quite different from actual
seismic survey sounds or even
reasonable surrogates. However, Payne
et al. (2009) reported no statistical
differences in mortality/morbidity
between control and exposed groups of
capelin eggs or monkfish larvae. Saetre
and Ona (1996) applied a ‘worst-case
scenario’ mathematical model to
investigate the effects of seismic energy
on fish eggs and larvae. They concluded
that mortality rates caused by exposure
to seismic surveys are so low, as
compared to natural mortality rates, that
the impact of seismic surveying on
recruitment to a fish stock must be
regarded as insignificant.
Physiological Effects—Physiological
effects refer to cellular and/or
biochemical responses of fish to
acoustic stress. Such stress potentially
could affect fish populations by
increasing mortality or reducing
reproductive success. Primary and
secondary stress responses of fish after
exposure to seismic survey sound
appear to be temporary in all studies
done to date (Sverdrup et al., 1994;
Santulli et al., 1999; McCauley et al.,
2000a, b). The periods necessary for the
biochemical changes to return to normal
are variable and depend on numerous
aspects of the biology of the species and
of the sound stimulus.
Behavioral Effects—Behavioral effects
include changes in the distribution,
migration, mating, and catchability of
fish populations. Studies investigating
the possible effects of sound (including
seismic survey sound) on fish behavior
have been conducted on both uncaged
and caged individuals (e.g., Chapman
and Hawkins, 1969; Pearson et al., 1992;
Santulli et al., 1999; Wardle et al., 2001;
Hassel et al., 2003). Typically, in these
studies fish exhibited a sharp startle
response at the onset of a sound
followed by habituation and a return to
normal behavior after the sound ceased.
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The Minerals Management Service
(MMS, 2005) assessed the effects of a
proposed seismic survey in Cook Inlet.
The seismic survey proposed using
three vessels, each towing two, fourairgun arrays ranging from 1,500 to
2,500 in3. MMS noted that the impact to
fish populations in the survey area and
adjacent waters would likely be very
low and temporary. MMS also
concluded that seismic surveys may
displace the pelagic fishes from the area
temporarily when airguns are in use.
However, fishes displaced and avoiding
the airgun noise are likely to backfill the
survey area in minutes to hours after
cessation of seismic testing. Fishes not
dispersing from the airgun noise (e.g.,
demersal species) may startle and move
short distances to avoid airgun
emissions.
In general, any adverse effects on fish
behavior or fisheries attributable to
seismic testing may depend on the
species in question and the nature of the
fishery (season, duration, fishing
method). They may also depend on the
age of the fish, its motivational state, its
size, and numerous other factors that are
difficult, if not impossible, to quantify at
this point, given such limited data on
effects of airguns on fish, particularly
under realistic at-sea conditions.
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Anticipated Effects on Invertebrates
The existing body of information on
the impacts of seismic survey sound on
marine invertebrates is very limited.
However, there is some unpublished
and very limited evidence of the
potential for adverse effects on
invertebrates, thereby justifying further
discussion and analysis of this issue.
The three types of potential effects of
exposure to seismic surveys on marine
invertebrates are pathological,
physiological, and behavioral. Based on
the physical structure of their sensory
organs, marine invertebrates appear to
be specialized to respond to particle
displacement components of an
impinging sound field and not to the
pressure component (Popper et al.,
2001).
The only information available on the
impacts of seismic surveys on marine
invertebrates involves studies of
individuals; there have been no studies
at the population scale. Thus, available
information provides limited insight on
possible real-world effects at the
regional or ocean scale. The most
important aspect of potential impacts
concerns how exposure to seismic
survey sound ultimately affects
invertebrate populations and their
viability, including availability to
fisheries.
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Literature reviews of the effects of
seismic and other underwater sound on
invertebrates were provided by
Moriyasu et al. (2004) and Payne et al.
(2008). The following sections provide a
synopsis of available information on the
effects of exposure to seismic survey
sound on species of decapod
crustaceans and cephalopods, the two
taxonomic groups of invertebrates on
which most such studies have been
conducted. The available information is
from studies with variable degrees of
scientific soundness and from anecdotal
information. A more detailed review of
the literature on the effects of seismic
survey sound on invertebrates is
provided in Appendix D of NSF/USGS’s
PEIS.
Pathological Effects—In water, lethal
and sub-lethal injury to organisms
exposed to seismic survey sound
appears to depend on at least two
features of the sound source: (1) The
received peak pressure; and (2) the time
required for the pressure to rise and
decay. Generally, as received pressure
increases, the period for the pressure to
rise and decay decreases, and the
chance of acute pathological effects
increases. For the type of airgun array
planned for the proposed program, the
pathological (mortality) zone for
crustaceans and cephalopods is
expected to be within a few meters of
the seismic source, at most; however,
very few specific data are available on
levels of seismic signals that might
damage these animals. This premise is
based on the peak pressure and rise/
decay time characteristics of seismic
airgun arrays currently in use around
the world.
Some studies have suggested that
seismic survey sound has a limited
pathological impact on early
developmental stages of crustaceans
(Pearson et al., 1994; Christian et al.,
2003; DFO, 2004). However, the impacts
appear to be either temporary or
insignificant compared to what occurs
under natural conditions. Controlled
field experiments on adult crustaceans
(Christian et al., 2003, 2004; DFO, 2004)
and adult cephalopods (McCauley et al.,
2000a, b) exposed to seismic survey
sound have not resulted in any
significant pathological impacts on the
animals. It has been suggested that
exposure to commercial seismic survey
activities has injured giant squid
(Guerra et al., 2004), but the article
provides little evidence to support this
claim. Tenera Environmental (2011b)
reported that Norris and Mohl (1983,
summarized in Mariyasu et al., 2004)
observed lethal effects in squid (Loligo
vulgaris) at levels of 246 to 252 dB after
3 to 11 minutes.
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Andre et al. (2011) exposed four
species of cephalopods (Loligo vulgaris,
Sepia officinalis, Octopus vulgaris, and
Ilex coindetii), primarily cuttlefish, to
two hours of continuous 50 to 400 Hz
sinusoidal wave sweeps at 157±5 dB re
1 mPa while captive in relatively small
tanks. They reported morphological and
ultrastructural evidence of massive
acoustic trauma (i.e., permanent and
substantial alterations [lesions] of
statocyst sensory hair cells) to the
exposed animals that increased in
severity with time, suggesting that
cephalopods are particularly sensitive to
low frequency sound. The received SPL
was reported as 157±5 dB re 1 mPa, with
peak levels at 175 dB re 1 mPa. As in the
McCauley et al. (2003) paper on sensory
hair cell damage in pink snapper as a
result of exposure to seismic sound, the
cephalopods were subjected to higher
sound levels than they would be under
natural conditions, and they were
unable to swim away from the sound
source.
Physiological Effects—Physiological
effects refer mainly to biochemical
responses by marine invertebrates to
acoustic stress. Such stress potentially
could affect invertebrate populations by
increasing mortality or reducing
reproductive success. Primary and
secondary stress responses (i.e., changes
in haemolymph levels of enzymes,
proteins, etc.) of crustaceans have been
noted several days or months after
exposure to seismic survey sounds
(Payne et al., 2007). It was noted
however, than no behavioral impacts
were exhibited by crustaceans (Christian
et al., 2003, 2004; DFO, 2004). The
periods necessary for these biochemical
changes to return to normal are variable
and depend on numerous aspects of the
biology of the species and of the sound
stimulus.
Behavioral Effects—There is
increasing interest in assessing the
possible direct and indirect effects of
seismic and other sounds on
invertebrate behavior, particularly in
relation to the consequences for
fisheries. Changes in behavior could
potentially affect such aspects as
reproductive success, distribution,
susceptibility to predation, and
catchability by fisheries. Studies
investigating the possible behavioral
effects of exposure to seismic survey
sound on crustaceans and cephalopods
have been conducted on both uncaged
and caged animals. In some cases,
invertebrates exhibited startle responses
(e.g., squid in McCauley et al., 2000a, b).
In other cases, no behavioral impacts
were noted (e.g., crustaceans in
Christian et al., 2003, 2004; DFO 2004).
There have been anecdotal reports of
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reduced catch rates of shrimp shortly
after exposure to seismic surveys;
however, other studies have not
observed any significant changes in
shrimp catch rate (Andriguetto-Filho et
al., 2005). Similarly, Parry and Gason
(2006) did not find any evidence that
lobster catch rates were affected by
seismic surveys. Any adverse effects on
crustacean and cephalopod behavior or
fisheries attributable to seismic survey
sound depend on the species in
question and the nature of the fishery
(season, duration, fishing method).
Proposed Mitigation
In order to issue an Incidental Take
Authorization (ITA) under section
101(a)(5)(D) of the MMPA, NMFS must
set forth the permissible methods of
taking pursuant to such activity, and
other means of effecting the least
practicable impact on such species or
stock and its habitat, paying particular
attention to rookeries, mating grounds,
and areas of similar significance, and
the availability of such species or stock
for taking for certain subsistence uses.
NSF and ASC reviewed the following
source documents and have
incorporated a suite of appropriate
mitigation measures into their project
description.
(1) Protocols used during previous
NSF and USGS-funded seismic research
cruises as approved by NMFS and
detailed in the recently completed
‘‘Final Programmatic Environmental
Impact Statement/Overseas
Environmental Impact Statement for
Marine Seismic Research Funded by the
National Science Foundation or
Conducted by the U.S. Geological
Survey;’’
(2) Previous IHA applications and
IHAs approved and authorized by
NMFS; and
(3) Recommended best practices in
Richardson et al. (1995), Pierson et al.
(1998), and Weir and Dolman, (2007).
To reduce the potential for
disturbance from acoustic stimuli
associated with the activities, NSF, ASC
and/or its designees have proposed to
implement the following mitigation
measures for marine mammals:
(1) Proposed exclusion zones around
the sound source;
(2) Speed and course alterations;
(3) Shut-down procedures; and
(4) Ramp-up procedures.
Proposed Exclusion Zones—During
pre-planning of the cruise, the smallest
airgun array was identified that could be
used and still meet the geophysical
scientific objectives. NSF and ASC use
radii to designate exclusion and buffer
zones and to estimate take for marine
mammals. Table 2 (presented earlier in
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this document) shows the distances at
which one would expect to receive three
sound levels (160, 180, and 190 dB)
from the two GI airgun array. The 180
and 190 dB level shut-down criteria are
applicable to cetaceans and pinnipeds,
respectively, as specified by NMFS
(2000). NSF and ASC used these levels
to establish the exclusion and buffer
zones.
Received sound levels have been
modeled by L–DEO for a number of
airgun configurations, including two 45
in3 Nucleus G airguns, in relation to
distance and direction from the airguns
(see Figure 2 of the IHA application). In
addition, propagation measurements of
pulses from two GI airguns have been
reported for shallow water
(approximately 30 m [98.4 ft] depth in
the GOM (Tolstoy et al., 2004).
However, measurements were not made
for the two GI airguns in deep water.
The model does not allow for bottom
interactions, and is most directly
applicable to deep water. Based on the
modeling, estimates of the maximum
distances from the GI airguns where
sound levels are predicted to be 190,
180, and 160 dB re 1 mPa (rms) in
shallow, intermediate, and deep water
were determined (see Table 2 above).
Empirical data concerning the 190,
180, and 160 dB (rms) distances were
acquired for various airgun arrays based
on measurements during the acoustic
verification studies conducted by L–
DEO in the northern GOM in 2003
(Tolstoy et al., 2004) and 2007 to 2008
(Tolstoy et al., 2009). Results of the 36
airgun array are not relevant for the two
GI airguns to be used in the proposed
survey. The empirical data for the 6, 10,
12, and 20 airgun arrays indicate that,
for deep water, the L–DEO model tends
to overestimate the received sound
levels at a given distance (Tolstoy et al.,
2004). Measurements were not made for
the two GI airgun array in deep water;
however, NSF and ASC propose to use
the safety radii predicted by L–DEO’s
model for the proposed GI airgun
operations in shallow, intermediate, and
deep water, although they are likely
conservative given the empirical results
for the other arrays.
Based on the modeling data, the
outputs from the pair of 45 in3 or 105
in3 GI airguns proposed to be used
during the seismic survey are
considered a low-energy acoustic source
in the NSF/USGS PEIS (2011) for
marine seismic research. A low-energy
seismic source was defined in the NSF/
USGS PEIS as an acoustic source whose
received level at 100 m is less than 180
dB. The NSF/USGS PEIS also
established for these low-energy
sources, a standard exclusion zone of
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487
100 m for all low-energy sources in
water depths greater than 100 m. This
standard 100 m exclusion zone would
be used during the proposed low-energy
seismic survey. The 180 and 190 dB
(rms) radii are shut-down criteria
applicable to cetaceans and pinnipeds,
respectively, as specified by NMFS
(2000); these levels were used to
establish exclusion zones. Therefore, the
assumed 180 and 190 dB radii are 100
m for intermediate and deep water,
respectively. If the PSO detects a marine
mammal(s) within or about to enter the
appropriate exclusion zone, the airguns
will be shut-down immediately.
Speed and Course Alterations—If a
marine mammal is detected outside the
exclusion zone and, based on its
position and direction of travel (relative
motion), is likely to enter the exclusion
zone, changes of the vessel’s speed and/
or direct course will be considered if
this does not compromise operational
safety or damage the deployed
equipment. This would be done if
operationally practicable while
minimizing the effect on the planned
science objectives. For marine seismic
surveys towing large streamer arrays,
however, course alterations are not
typically implemented due to the
vessel’s limited maneuverability. After
any such speed and/or course alteration
is begun, the marine mammal activities
and movements relative to the seismic
vessel will be closely monitored to
ensure that the marine mammal does
not approach within the exclusion zone.
If the marine mammal appears likely to
enter the exclusion zone, further
mitigation actions will be taken,
including further speed and/or course
alterations, and/or shut-down of the
airgun(s). Typically, during seismic
operations, the source vessel is unable
to change speed or course, and one or
more alternative mitigation measures
will need to be implemented.
Shut-down Procedures—NSF and
ASC will shut-down the operating
airgun(s) if a marine mammal is
detected outside the exclusion zone for
the airgun(s), and if the vessel’s speed
and/or course cannot be changed to
avoid having the animal enter the
exclusion zone, the seismic source will
be shut-down before the animal is
within the exclusion zone. Likewise, if
a marine mammal is already within the
exclusion zone when first detected, the
seismic source will be shut-down
immediately.
Following a shut-down, NSF and ASC
will not resume airgun activity until the
marine mammal has cleared the
exclusion zone. NSF and ASC will
consider the animal to have cleared the
exclusion zone if:
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• A PSO has visually observed the
animal leave the exclusion zone, or
• A PSO has not sighted the animal
within the exclusion zone for 15
minutes for species with shorter dive
durations (i.e., small odontocetes and
pinnipeds), or 30 minutes for species
with longer dive durations (i.e.,
mysticetes and large odontocetes,
including sperm, pygmy and dwarf
sperm, killer, and beaked whales).
Although power-down procedures are
often standard operating practice for
seismic surveys, they are not proposed
to be used during this planned seismic
survey because powering-down from
two airguns to one airgun would make
only a small difference in the exclusion
zone(s)—but probably not enough to
allow continued one-airgun operations
if a marine mammal came within the
exclusion zone for two airguns.
Ramp-up Procedures—Ramp-up of an
airgun array provides a gradual increase
in sound levels, and involves a stepwise increase in the number and total
volume of airguns firing until the full
volume of the airgun array is achieved.
The purpose of a ramp-up is to ‘‘warn’’
marine mammals in the vicinity of the
airguns and to provide the time for them
to leave the area avoiding any potential
injury or impairment of their hearing
abilities. NSF and ASC will follow a
ramp-up procedure when the airgun
array begins operating after a specified
period without airgun operations or
when a shut-down shut down has
exceeded that period. NSF and ASC
propose that, for the present cruise, this
period would be approximately 15
minutes. SIO, L–DEO, and USGS have
used similar periods (approximately 15
minutes) during previous low-energy
seismic surveys.
Ramp-up will begin with a single GI
airgun (45 or 105 in3). The second GI
airgun (45 or 105 in3) will be added after
5 minutes. During ramp-up, the PSOs
will monitor the exclusion zone, and if
marine mammals are sighted, a shutdown will be implemented as though
both GI airguns were operational.
If the complete exclusion zone has not
been visible for at least 30 minutes prior
to the start of operations in either
daylight or nighttime, NSF and ASC
will not commence the ramp-up. Given
these provisions, it is likely that the
airgun array will not be ramped-up from
a complete shut-down at night or in
thick fog, because the outer part of the
exclusion zone for that array will not be
visible during those conditions. If one
airgun has operated, ramp-up to full
power will be permissible at night or in
poor visibility, on the assumption that
marine mammals will be alerted to the
approaching seismic vessel by the
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sounds from the single airgun and could
move away if they choose. A ramp-up
from a shut-down may occur at night,
but only where the exclusion zone is
small enough to be visible. NSF and
ASC will not initiate a ramp-up of the
airguns if a marine mammal is sighted
within or near the applicable exclusion
zones during the day or close to the
vessel at night.
NMFS has carefully evaluated the
applicant’s proposed mitigation
measures and has considered a range of
other measures in the context of
ensuring that NMFS prescribes the
means of effecting the least practicable
adverse impact on the affected marine
mammal species and stocks and their
habitat. NMFS’s evaluation of potential
measures included consideration of the
following factors in relation to one
another:
(1) The manner in which, and the
degree to which, the successful
implementation of the measure is
expected to minimize adverse impacts
to marine mammals;
(2) The proven or likely efficacy of the
specific measure to minimize adverse
impacts as planned; and
(3) The practicability of the measure
for applicant implementation.
Based on NMFS’s evaluation of the
applicant’s proposed measures, as well
as other measures considered by NMFS
or recommended by the public, NMFS
has preliminarily determined that the
proposed mitigation measures provide
the means of effecting the least
practicable adverse impacts on marine
mammal species or stocks and their
habitat, paying particular attention to
rookeries, mating grounds, and areas of
similar significance.
Proposed Monitoring and Reporting
In order to issue an ITA for an
activity, section 101(a)(5)(D) of the
MMPA states that NMFS must set forth
‘‘requirements pertaining to the
monitoring and reporting of such
taking.’’ The MMPA implementing
regulations at 50 CFR 216.104 (a)(13)
indicate that requests for IHAs must
include the suggested means of
accomplishing the necessary monitoring
and reporting that will result in
increased knowledge of the species and
of the level of taking or impacts on
populations of marine mammals that are
expected to be present in the action
area.
Proposed Monitoring
NSF and ASC proposes to sponsor
marine mammal monitoring during the
proposed project, in order to implement
the proposed mitigation measures that
require real-time monitoring, and to
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satisfy the anticipated monitoring
requirements of the IHA. NSF and
ASC’s proposed ‘‘Monitoring Plan’’ is
described below this section. NSF and
ASC understand that this monitoring
plan will be subject to review by NMFS
and that refinements may be required.
The monitoring work described here has
been planned as a self-contained project
independent of any other related
monitoring projects that may be
occurring simultaneously in the same
regions. NSF and ASC is prepared to
discuss coordination of their monitoring
program with any related work that
might be done by other groups insofar
as this is practical and desirable.
Vessel-Based Visual Monitoring
PSOs will be based aboard the seismic
source vessel and will watch for marine
mammals near the vessel during
icebreaking activities, daytime airgun
operations (austral summer) and during
any ramp-ups of the airguns at night.
Nighttime operations of the airguns are
not anticipated. PSOs will also watch
for marine mammals near the seismic
vessel for at least 30 minutes prior to the
start of airgun operations and after an
extended shut-down (i.e., greater than
approximately 15 minutes for this
proposed low-energy seismic survey).
When feasible, PSOs will conduct
observations during daytime periods
when the seismic system is not
operating (such as during transits) for
comparison of sighting rates and
behavior with and without airgun
operations and between acquisition
periods. Based on PSO observations, the
airguns will be shut-down when marine
mammals are observed within or about
to enter a designated exclusion zone.
The exclusion zone is a region in which
a possibility exists of adverse effects on
animal hearing or other physical effects.
During seismic operations in the
Dumont d’Urville Sea of the Southern
Ocean, at least two PSOs will be based
aboard the Palmer. At least one PSO
will stand watch at all times while the
Palmer is operating airguns during the
proposed low-energy seismic survey;
this procedure will also be followed
when the vessel is conducting
icebreaking during transit. NSF and
ASC will appoint the PSOs with
NMFS’s concurrence. The lead PSO
would be experienced with marine
mammal species in the Southern Ocean,
the second PSO would receive
additional specialized training from the
PSO to ensure that they can identify
marine mammal species commonly
found in the Southern Ocean.
Observations will take place during
ongoing daytime operations and
nighttime ramp-ups of the airguns.
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During the majority of seismic
operations, at least one PSO will be on
duty from observation platforms (i.e.,
the best available vantage point on the
source vessel) to monitor marine
mammals near the seismic vessel.
PSO(s) will be on duty in shifts no
longer than 4 hours in duration. Other
crew will also be instructed to assist in
detecting marine mammals and
implementing mitigation requirements
(if practical). Before the start of the lowenergy seismic survey, the crew will be
given additional instruction on how to
do so. (Note: because of the high
latitude locations of the study areas,
twilight/darkness conditions are
expected to be limited to between 3 and
6 hours per day during the proposed
action.)
The Palmer is a suitable platform for
marine mammal observations and will
serve as the platform from which PSOs
will watch for marine mammals before
and during seismic operations. Two
locations are likely as observation
stations onboard the Palmer. Observing
stations are located on the bridge level,
with the PSO eye level at approximately
16.5 m (54.1 ft) above the waterline and
the PSO would have a good view
around the entire vessel. In addition,
there is an aloft observation tower for
the PSO approximately 24.4 m (80.1 ft)
above the waterline that is protected
from the weather, and affords PSOs an
even greater view. Standard equipment
for PSOs will be reticle binoculars.
Night-vision equipment will not be
available or required due to the constant
daylight conditions during the Antarctic
summer. The PSOs will be in
communication with ship’s officers on
the bridge and scientists in the vessel’s
operations laboratory, so they can
advise promptly of the need for
avoidance maneuvers or seismic source
shut-down. Observing stations will be at
the bridge level and the aloft
observation tower. The approximate
view around the vessel from the bridge
is 270° and 360° from the aloft
observation tower. During daytime, the
PSO(s) will scan the area around the
vessel systematically with reticle
binoculars (e.g., 7 × 50 Fujinon FMTRC–
SX) and the naked eye. These binoculars
will have a built-in daylight compass.
Estimating distances is done primarily
with the reticles in the binoculars. The
PSO(s) will be in direct (radio) wireless
communication with ship’s officers on
the bridge and scientists in the vessel’s
operations laboratory during seismic
operations, so they can advise the vessel
operator, science support personnel,
and the science party promptly of the
need for avoidance maneuvers or a shut-
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down of the seismic source. PSOs will
monitor for the presence pinnipeds and
cetaceans during icebreaking activities,
and will be limited to those marine
mammal species in proximity to the ice
margin habitat. Observations within the
buffer zone would also include
pinnipeds that may be present on the
surface of the sea ice (i.e., hauled-out)
and that could potentially dive into the
water as the vessel approaches,
indicating disturbance from noise
generated by icebreaking activities).
When marine mammals are detected
within or about to enter the designated
exclusion zone, the airguns will
immediately be shut-down if necessary.
The PSO(s) will continue to maintain
watch to determine when the animal(s)
are outside the exclusion zone by visual
confirmation. Airgun operations will
not resume until the animal is
confirmed to have left the exclusion
zone, or if not observed after 15 minutes
for species with shorter dive durations
(small odontocetes and pinnipeds) or 30
minutes for species with longer dive
durations (mysticetes and large
odontocetes, including sperm, killer,
and beaked whales).
PSO Data and Documentation
PSOs will record data to estimate the
numbers of marine mammals exposed to
various received sound levels and to
document apparent disturbance
reactions or lack thereof. Data will be
used to estimate numbers of animals
potentially ‘‘taken’’ by harassment (as
defined in the MMPA). They will also
provide information needed to order a
shut-down of the airguns when a marine
mammal is within or near the exclusion
zone. Observations will also be made
during icebreaking activities as well as
daytime periods when the Palmer is
underway without seismic operations
(i.e., transits, to, from, and through the
study area) to collect baseline biological
data.
When a sighting is made, the
following information about the sighting
will be recorded:
1. Species, group size, age/size/sex
categories (if determinable), behavior
when first sighted and after initial
sighting, heading (if consistent), bearing
and distance from seismic vessel,
sighting cue, apparent reaction to the
seismic source or vessel (e.g., none,
avoidance, approach, paralleling, etc.),
and behavioral pace.
2. Time, location, heading, speed,
activity of the vessel, sea state, wind
force, visibility, and sun glare.
The data listed under (2) will also be
recorded at the start and end of each
observation watch, and during a watch
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489
whenever there is a change in one or
more of the variables.
All observations, as well as
information regarding ramp-ups or shutdowns will be recorded in a
standardized format. Data will be
entered into an electronic database. The
data accuracy will be verified by
computerized data validity checks as
the data are entered and by subsequent
manual checking of the database by the
PSOs at sea. These procedures will
allow initial summaries of data to be
prepared during and shortly after the
field program, and will facilitate transfer
of the data to statistical, graphical, and
other programs for further processing
and archiving.
Results from the vessel-based
observations will provide the following
information:
1. The basis for real-time mitigation
(airgun shut-down).
2. Information needed to estimate the
number of marine mammals potentially
taken by harassment, which must be
reported to NMFS.
3. Data on the occurrence,
distribution, and activities of marine
mammals in the area where the seismic
study is conducted.
4. Information to compare the
distance and distribution of marine
mammals relative to the source vessel at
times with and without seismic activity.
5. Data on the behavior and
movement patterns of marine mammals
seen at times with and without seismic
activity.
NSF and ASC will submit a
comprehensive report to NMFS within
90 days after the end of the cruise. The
report will describe the operations that
were conducted and sightings of marine
mammals near the operations. The
report submitted to NMFS will provide
full documentation of methods, results,
and interpretation pertaining to all
monitoring. The 90-day report will
summarize the dates and locations of
seismic operations and all marine
mammal sightings (i.e., dates, times,
locations, activities, and associated
seismic survey activities). The report
will minimally include:
• Summaries of monitoring effort—
total hours, total distances, and
distribution of marine mammals
through the study period accounting for
Beaufort sea state and other factors
affecting visibility and detectability of
marine mammals;
• Analyses of the effects of various
factors influencing detectability of
marine mammals including Beaufort sea
state, number of PSOs, and fog/glare;
• Species composition, occurrence,
and distribution of marine mammals
sightings including date, water depth,
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numbers, age/size/gender, and group
sizes; and analyses of the effects of
seismic operations;
• Sighting rates of marine mammals
during periods with and without airgun
activities (and other variables that could
affect detectability);
• Initial sighting distances versus
airgun activity state;
• Closest point of approach versus
airgun activity state;
• Observed behaviors and types of
movements versus airgun activity state;
• Numbers of sightings/individuals
seen versus airgun activity state; and
• Distribution around the source
vessel versus airgun activity state.
The report will also include estimates
of the number and nature of exposures
that could result in ‘‘takes’’ of marine
mammals by harassment or in other
ways. After the report is considered
final, it will be publicly available on the
NMFS Web site at: https://
www.nmfs.noaa.gov/pr/permits/
incidental.htm#iha.
In the unanticipated event that the
specified activity clearly causes the take
of a marine mammal in a manner
prohibited by this IHA, such as an
injury (Level A harassment), serious
injury or mortality (e.g., ship-strike, gear
interaction, and/or entanglement), NSF
and ASC will immediately cease the
specified activities and immediately
report the incident to the Chief of the
Permits and Conservation Division,
Office of Protected Resources, NMFS at
301–427–8401 and/or by email to
Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report
must include the following information:
• Time, date, and location (latitude/
longitude) of the incident;
• Name and type of vessel involved;
• Vessel’s speed during and leading
up to the incident;
• Description of the incident;
• Status of all sound source use in the
24 hours preceding the incident;
• Water depth;
• Environmental conditions (e.g.,
wind speed and direction, Beaufort sea
state, cloud cover, and visibility);
• Description of all marine mammal
observations in the 24 hours preceding
the incident;
• Species identification or
description of the animal(s) involved;
• Fate of the animal(s); and
• Photographs or video footage of the
animal(s) (if equipment is available).
Activities shall not resume until
NMFS is able to review the
circumstances of the prohibited take.
NMFS shall work with NSF and ASC to
determine what is necessary to
minimize the likelihood of further
prohibited take and ensure MMPA
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compliance. NSF and ASC may not
resume their activities until notified by
NMFS via letter or email, or telephone.
In the event that NSF and ASC
discovers an injured or dead marine
mammal, and the lead PSO determines
that the cause of the injury or death is
unknown and the death is relatively
recent (i.e., in less than a moderate state
of decomposition as described in the
next paragraph), NSF and ASC will
immediately report the incident to the
Chief of the Permits and Conservation
Division, Office of Protected Resources,
NMFS, at 301–427–8401, and/or by
email to Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report
must include the same information
identified in the paragraph above.
Activities may continue while NMFS
reviews the circumstances of the
incident. NMFS will work with NSF
and ASC to determine whether
modifications in the activities are
appropriate.
In the event that NSF and ASC
discovers an injured or dead marine
mammal, and the lead PSO determines
that the injury or death is not associated
with or related to the activities
authorized in the IHA (e.g., previously
wounded animal, carcass with moderate
or advanced decomposition, or
scavenger damage), NSF and ASC will
report the incident to the Chief of the
Permits and Conservation Division,
Office of Protected Resources, NMFS, at
301–427–8401, and/or by email to
Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov, within 24
hours of discovery. NSF and ASC will
provide photographs or video footage (if
available) or other documentation of the
stranded animal sighting to NMFS.
Activities may continue while NMFS
reviews the circumstances of the
incident.
Estimated Take by Incidental
Harassment
Except with respect to certain
activities not pertinent here, the MMPA
defines ‘‘harassment’’ as: any act of
pursuit, torment, or annoyance which (i)
has the potential to injure a marine
mammal or marine mammal stock in the
wild [Level A harassment]; or (ii) has
the potential to disturb a marine
mammal or marine mammal stock in the
wild by causing disruption of behavioral
patterns, including, but not limited to,
migration, breathing, nursing, breeding,
feeding, or sheltering [Level B
harassment].
Level B harassment is anticipated and
proposed to be authorized as a result of
the proposed low-energy marine seismic
survey in the Dumont d’Urville Sea off
the coast of East Antarctica. Acoustic
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stimuli (i.e., increased underwater
sound) generated during the operation
of the seismic airgun array and
icebreaking activities are expected to
result in the behavioral disturbance of
some marine mammals. There is no
evidence that the planned activities
could result in injury, serious injury, or
mortality for which NSF and ASC seeks
the IHA. The required mitigation and
monitoring measures will minimize any
potential risk for injury, serious injury,
or mortality.
The following sections describe NSF
and ASC’s methods to estimate take by
incidental harassment and present the
applicant’s estimates of the numbers of
marine mammals that could be affected
during the proposed low-energy seismic
survey in the Dumont d’Urville Sea off
the coast of East Antarctica. The
estimates are based on a consideration
of the number of marine mammals that
could be harassed by approximately
2,800 km (1511.9 nmi) of seismic
operations with the two GI airgun array
to be used and 1,000 km of icebreaking
activities.
During simultaneous operations of the
airgun array and the other sound
sources, any marine mammals close
enough to be affected by the single and
multi-beam echosounders, pingers,
ADCP, sub-bottom profiler, etc. would
already be affected by the airguns.
During times when the airguns are not
operating, it is unlikely that marine
mammals will exhibit more than minor,
short-term responses to the
echosounders, ADCPs, and sub-bottom
profiler given their characteristics (e.g.,
narrow, downward-directed beam) and
other considerations described
previously. Therefore, for this activity,
take was not authorized specifically for
these sound sources beyond that which
is already authorized for airguns and
icebreaking activities.
There are no stock assessments and
very limited population information
available for marine mammals in the
Dumont d’Urville Sea. Sighting data
from the Australian Antarctic Division’s
(AAD) BROKE-West surveys (Southwell
et al., 2008; 2012) was used to
determine and estimate marine
mammals densities for mysticetes and
odontocetes and AAD data components
for pinnipeds, which were not available
for the proposed seismic survey’s action
area in the Dumont d’Urville Sea. While
population density data for cetaceans in
the Southern Ocean is sparse to
nonexistent, reported sightings data
from previous research cruises suggest
cetaceans such as those identified in
Table 12 of the IHA application span a
range greater than 4,000 km (2,159.8
nmi) off the coast of East Antarctica.
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
The AAD BROKE-West survey was not
specifically designed to quantify marine
mammals. The data was in terms of
animals sighted per time unit, and this
sighting data was then converted to an
areal density by multiplying the number
of animals observed by the estimated
area observed during the survey. As
such, some marine mammals that were
present in the area may not have been
observed.
The estimated number of cetaceans
and pinnipeds that may be potentially
exposed from the proposed seismic
airgun operations and icebreaking
activities based on sighting data from
previous research cruises over a 52-day
period and 13-day period. Some of the
AAD sighting data was used as the basis
for estimating take included
‘‘unidentified whale’’ species, this
category was retained and pro-rated to
the other species because environmental
conditions may be present during the
proposed action to limit identification
of observed cetaceans. The estimated
frequency of sightings data for cetaceans
incorporates a correction factor of 5 that
assumes only 20% of the animals
present were reported due to sea ice and
other conditions that may have
hindered observation. The 20% factor
was intended to conservatively account
for this. Conservatively, a 40%
correction factor was used for
pinnipeds. The expected sightings data
incorporates a 40% correction factor to
account for seals that may be in the
water versus those hauled-out on ice
tkelley on DSK3SPTVN1PROD with NOTICES2
Species
Mysticetes:
Southern right whale .............
Humpback whale ..................
Antarctic minke whale ...........
Sei whale ..............................
Fin whale ..............................
Blue whale ............................
Odontocetes:
Sperm whale .........................
Arnoux’s beaked whale ........
Cuvier’s beaked whale .........
Southern bottlenose beaked
whale.
Killer whale ...........................
Long-finned pilot whale .........
Hourglass dolphin .................
Spectacled porpoise .............
Pinnipeds:
Crabeater seal ......................
Reported
sightings 1 2
*sightings
have been
pro-rated to
include
unidentified
animals*
surface. This correction factor for
pinnipeds was conservatively based on
Southwell et al. (2012), which estimated
20 to 40% of crabeater seals may be in
the water in a particular area while the
rest are hauled-out. The correction
factor takes into consideration some
pinnipeds may not be observed due to
poor visibility conditions.
Sightings data were collected by the
AAD; however, the AAD methodology
was not described. Density is generally
reported in the number of animals per
km or square km. Estimated area
observed by observers was calculated by
using the average vessel speed (5.6 km/
hr) times the estimated hours of the
survey to estimate the total distance
covered for each of the surveys. This
was then converted from the linear
distance into an area by assuming a
width of 5 km that could be reliably
visually surveyed. Therefore, the
estimated area was 5,753 km2 (1,677.3
nmi2) to obtain mysticete and
odontocete densities and the estimated
area was 1,419 km2 (413.7 nmi2) to
obtain pinniped densities.
Of the six species of pinnipeds that
may be present in the study area during
the proposed action, only four species
are expected to be observed and occur
mostly near pack ice or coastal areas
and not prevalent in open sea areas
where the low-energy seismic survey
would be conducted. Because density
estimates for pinnipeds in that Antarctic
regions typically represent individuals
that have hauled-out of the water, those
Corrected
sightings
(assume 20%
for cetaceans,
40% of
pinnipeds in
water)
Density inwater
[density inwater and/or
on-ice]
(#/km) 2
estimates are not representative of
individuals that are in the water and
could be potentially exposed to
underwater sounds during the seismic
airgun operations and icebreaking
activities; therefore, the pinniped
densities have been adjusted to account
for this concern. Take was not requested
for southern elephant seals and
Antarctic fur seals because preferred
habitat for these species is not within
the proposed action area. Although no
sightings of Weddell seals and
spectacled porpoises were reported in
the BROKE-West sighting data, take was
requested for these species based on
NMFS recommendation and IWC
SOWER data. Although there is some
uncertainty about the representatives of
the data and the assumptions used in
the calculations below, the approach
used here is believed to be the best
available approach.
Table 5. Estimated densities and
possible number of marine mammal
species that might be exposed to greater
than or equal to 120 dB (icebreaking)
and 160 dB (airgun operations) during
NSF and ASC’s proposed low-energy
seismic survey (approximately 1,000 km
of tracklines/approximately 3,500 km2
ensonified area for icebreaking activities
and approximately 2,800 km of
tracklines/approximately 5,628 km2
ensonified area for airgun operations) in
the Dumont d’Urville Sea of the
Southern Ocean, February to March
2014.
Calculated
take from
seismic airgun
operations
(i.e., estimated
number of
individuals
exposed to
sound levels
≥160 dB re 1
μPa) 3
Calculated
take from
icebreaking
activities (i.e.,
estimated
number of
individuals
exposed to
sound levels
≥120 dB re 1
μPa) 4
Approximate
percentage of
population
estimate
(calculated
total take) 5
0
238
136
4
232
2
0
1,190
680
20
1,160
10
0
0.2068400
0.1181943
0.0034763
0.2016255
0.0017382
0
1,165
666
20
1,135
10
0
724
414
13
706
7
NA
5.4
0.4
0.04
1.3
1.0
32
0
0
0
160
0
0
0
0.0278104
0
0
0
157
0
0
0
98
0
0
0
2.7
NA
NA
NA
62
24
27
26
310
120
135
130
0.538827
0.0208578
0.0234650
0.0225690
304
118
133
128
189
74
83
80
2.0
0.1
0.15
NA
2,220
888
3,521
7,663
0.2
Leopard seal .........................
17
7
27
59
0.04
Ross seal ..............................
42
17
0.625546
[2.189411]
0.00479
[0.016766]
0.011835
[0.041421]
66
145
0.2
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03JAN2
Total requested take
authorization 6
0.
1,165 + 724 = 1,889.
666 + 414 = 1,080.
20 + 13 = 33.
1,135 + 706 = 1,841.
10 + 7 = 17.
157 + 98 = 255.
0.
0.
0.
304
118
133
128
+
+
+
+
189 = 493.
74 = 192.
83 = 216.
80 = 208.
3,521 + 7,663 = 11,184.
27 + 59 = 86.
66 + 145 = 211.
492
Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
Species
Reported
sightings 1 2
*sightings
have been
pro-rated to
include
unidentified
animals*
Corrected
sightings
(assume 20%
for cetaceans,
40% of
pinnipeds in
water)
Weddell seal .........................
302
121
Southern elephant seal .........
Antarctic fur seal ...................
0
0
0
0
Density inwater
[density inwater and/or
on-ice]
(#/km) 2
Calculated
take from
seismic airgun
operations
(i.e., estimated
number of
individuals
exposed to
sound levels
≥160 dB re 1
μPa) 3
Calculated
take from
icebreaking
activities (i.e.,
estimated
number of
individuals
exposed to
sound levels
≥120 dB re 1
μPa) 4
Approximate
percentage of
population
estimate
(calculated
total take) 5
303
189
0.1
303 + 189 = 492.
0
0
0
0
NA
NA
0.
0.
0.054
[0.054]
0
0
Total requested take
authorization 6
tkelley on DSK3SPTVN1PROD with NOTICES2
NA = Not available or not assessed.
1 Sightings from a 52 day (5,753 km2) period on the AAD BROKE-West survey during January to March 2006.
2 Sightings December 3 to 16, 1999 (1,420 km2 and 75,564 km2), below 60° South latitude between 110 to 165° East longitude. All sightings were animals hauledout of the water and on the sea ice.
3 Calculated take is estimated density (reported density times correction factor) multiplied by the area ensonified to 160 dB (rms) around the planned seismic lines,
increased by 25% for contingency.
4 Calculated take is estimated density (reported density) multiplied by the area ensonified to 120 dB (rms) around the planned transit lines where icebreaking activities may occur.
5 Total requested (and calculated) takes expressed as percentages of the species or regional populations.
6 Requested Take Authorization includes unidentified animals that were added to the observed and identified species on a pro-rated basis.
Note: Take was not requested for southern elephant seals and Antarctic fur seals because preferred habitat for these species is not within the proposed action
area.
Icebreaking in Antarctic waters will
occur, as necessary, between the
latitudes of approximately 66 to 70°
South and between 140 and 165° East.
Based on a maximum sea ice extent of
250 km and estimating that the Palmer
will transit to the innermost shelf and
back into open water twice—a round
trip transit in each of the potential work
regions, it is estimated that the Palmer
will actively break ice up to a distance
of 1,000 km. Based on the ship’s speed
of 5 kts under moderate ice conditions,
this distance represents approximately
108 hrs of icebreaking operations. This
calculation is likely an overestimation
because icebreakers often follow leads
when they are available and thus do not
break ice at all times.
Numbers of marine mammals that
might be present and potentially
disturbed are estimated based on the
available data about marine mammal
distribution and densities in the
Southern Ocean study are during the
austral summer. NSF and ASC
estimated the number of different
individuals that may be exposed to
airgun sounds with received levels
greater than or equal to 160 dB re 1 mPa
(rms) for seismic airgun operations and
greater than or equal to 120 dB re 1 mPa
(rms) for icebreaking activities on one or
more occasions by considering the total
marine area that would be within the
160 dB radius around the operating
airgun array and 120 dB radius for the
icebreaking activities on at least one
occasion and the expected density of
marine mammals in the area (in the
absence of the a seismic survey and
icebreaking activities). The number of
possible exposures can be estimated by
considering the total marine area that
would be within the 160 dB radius (i.e.,
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diameter is 1,005 m times 2) around the
operating airguns. The ensonified area
for icebreaking was estimated by
multiplying the distance of the
icebreaking activities (1,000 km) by the
estimated diameter of the area within
the 120 dB radius (i.e., diameter is 1,750
m times 2). The 160 dB radii are based
on acoustic modeling data for the
airguns that may be used during the
proposed action (see Attachment B of
the IHA application). As summarized in
Table 2 (see Table 11 of the IHA
application), the modeling results for
the proposed low-energy seismic airgun
array indicate the received levels are
dependent on water depth. Since the
majority of the proposed airgun
operations would be conducted in
waters 100 to 1,000 m deep, the buffer
zone of 1,005 m used for the two 105 in3
GI airguns was used to be more
conservative. The expected sighting data
for pinnipeds accounts for both
pinnipeds that may be in the water and
those hauled-out on ice surfaces. While
the number of cetaceans that may be
encountered within the ice margin
habitat would be expected to be less
than open water, the estimates utilized
expected sightings for the open water
and represent conservative estimates. It
is unlikely that a particular animal
would stay in the area during the entire
survey.
The number of different individuals
potentially exposed to received levels
greater than or equal to 160 dB re 1 mPa
(rms) from seismic airgun operations
and 120 dB re 1 mPa (rms) for
icebreaking activities was calculated by
multiplying:
(1) The expected species density (in
number/km2), times.
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(2) The anticipated area to be
ensonified to that level during airgun
operations.
Applying the approach described
above, approximately 5,628 km2
(including the 25% contingency) would
be ensonified within the 160 dB
isopleth for seismic airgun operations
and approximately 3,500 km2 would be
ensonified within the 120 dB isopleth
for icebreaking activities on one or more
occasions during the proposed survey.
The take calculations within the study
sites do not explicitly add animals to
account for the fact that new animals
(i.e., turnover) are not accounted for in
the initial density snapshot and animals
could also approach and enter the area
ensonified above 160 dB for seismic
airgun operations and 120 dB for
icebreaking activities; however, studies
suggest that many marine mammals will
avoid exposing themselves to sounds at
this level, which suggests that there
would not necessarily be a large number
of new animals entering the area once
the seismic survey and icebreaking
activities started. Because this approach
for calculating take estimates does not
allow for turnover in the marine
mammal populations in the area during
the course of the survey, the actual
number of individuals exposed may be
underestimated, although the
conservative (i.e., probably
overestimated) line-kilometer distances
used to calculate the area may offset
this. Also, the approach assumes that no
cetaceans or pinnipeds will move away
or toward the tracklines as the Palmer
approaches in response to increasing
sound levels before the levels reach 160
dB for seismic airgun operations and
120 dB for icebreaking activities.
Another way of interpreting the
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estimates that follow is that they
represent the number of individuals that
are expected (in absence of a seismic
and icebreaking program) to occur in the
waters that will be exposed to greater
than or equal to 160 dB (rms) for seismic
airgun operations and greater than or
equal to 120 dB (rms) for icebreaking
activities.
NSF and ASC’s estimates of exposures
to various sound levels assume that the
proposed surveys will be carried out in
full; however, the ensonified areas
calculated using the planned number of
line-kilometers has been increased by
25% to accommodate lines that may
need to be repeated, equipment testing,
etc. As is typical during offshore ship
surveys, inclement weather and
equipment malfunctions are likely to
cause delays and may limit the number
of useful line-kilometers of seismic
operations that can be undertaken. The
estimates of the numbers of marine
mammals potentially exposed to 120 dB
(rms) and 160 dB (rms) received levels
are precautionary and probably
overestimate the actual numbers of
marine mammals that could be
involved. These estimates assume that
there will be no weather, equipment, or
mitigation delays, which is highly
unlikely.
Table 5 shows the estimates of the
number of different individual marine
mammals anticipated to be exposed to
greater than or equal to 120 dB re 1 mPa
(rms) for icebreaking activities and
greater than or equal to 160 dB re 1 mPa
(rms) for seismic airgun operations
during the seismic survey if no animals
moved away from the survey vessel. The
total requested take authorization is
given in the far right column of Table
5.
The estimate of the number of
individual cetaceans and pinnipeds that
could be exposed to seismic sounds
with received levels greater than or
equal to 160 dB re 1 mPa (rms) and
sounds from icebreaking activities with
received levels greater than or equal to
120 dB re 1 mPa (rms) during the
proposed survey is (with 25%
contingency) in Table 5 of this
document. That total (with 25%
contingency) includes 1,889 humpback,
1,080 Antarctic minke, 33 sei, 1,841 fin,
17 blue, and 255 sperm whales could be
taken by Level B harassment during the
proposed seismic survey, which would
represent 5.4, 0.4, 0.04, 1.3, 1, and 2.7%
of the worldwide or regional
populations, respectively. Some of the
cetaceans potentially taken by Level B
harassment are delphinids and
porpoises: killer whales, long-finned
pilot whales, hourglass dolphins, and
spectacled porpoises are estimated to be
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the most common delphinid and
porpoise species in the area, with
estimates of 493, 192, 216, and 208,
which would represent 2, 0.1, and
0.15% (spectacled porpoise population
is not available) of the affected
worldwide or regional populations,
respectively. Most of the pinnipeds
potentially taken by Level B harassment
are: Crabeater, leopard, Ross, and
Weddell seals with estimates of 11,184,
86, 211, and 492, which would
represent 0.2, 0.04, 0.2, and 0.1% of the
affected worldwide or regional
populations, respectively.
Encouraging and Coordinating
Research
NSF and ASC will coordinate the
planned marine mammal monitoring
program associated with the proposed
low-energy seismic survey with other
parties that express interest in this
activity and area. NSF and ASC will
coordinate with applicable U.S.
agencies (e.g., NMFS), and will comply
with their requirements. NSF has
already reached out to the Australian
Antarctic Division (AAD), who are the
proponents of the proposed marine
protected area and regularly conduct
research expeditions in the marine
environment off East Antarctica.
The proposed action would
complement fieldwork studying other
Antarctic ice shelves, oceanographic
studies, and ongoing development of ice
sheet and other ocean models. It would
facilitate learning at sea and ashore by
students, help to fill important spatial
and temporal gaps in a lightly sampled
region of coastal Antarctica, provide
additional data on marine mammals
present in the East Antarctic study
areas, and communicate its findings via
reports, publications and public
outreach.
Impact on Availability of Affected
Species or Stock for Taking for
Subsistence Uses
Section 101(a)(5)(D) of the MMPA
also requires NMFS to determine that
the authorization will not have an
unmitigable adverse effect on the
availability of marine mammal species
or stocks for subsistence use. There are
no relevant subsistence uses of marine
mammals in the study area (in the
Dumont d’Urville Sea off the coast of
East Antarctica) that implicate MMPA
section 101(a)(5)(D).
Negligible Impact and Small Numbers
Analysis Determination
As a preliminary matter, NMFS
typically includes our negligible impact
and small numbers analyses and
determinations under the same section
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493
heading of our Federal Register notices.
Despite co-locating these terms, NMFS
acknowledges that negligible impact
and small numbers are distinct
standards under the MMPA and treat
them as such. The analyses presented
below do not conflate the two standards;
instead, each standard has been
considered independently and NMFS
has applied the relevant factors to
inform our negligible impact and small
numbers determinations.
NMFS has defined ‘‘negligible
impact’’ in 50 CFR 216.103 as ‘‘an
impact resulting from the specified
activity that cannot be reasonably
expected to, and is not reasonably likely
to, adversely affect the species or stock
through effects on annual rates of
recruitment or survival.’’ In making a
negligible impact determination, NMFS
evaluated factors such as:
(1) The number of anticipated
injuries, serious injuries, or mortalities;
(2) The number, nature, and intensity,
and duration of Level B harassment (all
relatively limited); and
(3) The context in which the takes
occur (i.e., impacts to areas of
significance, impacts to local
populations, and cumulative impacts
when taking into account successive/
contemporaneous actions when added
to baseline data);
(4) The status of stock or species of
marine mammals (i.e., depleted, not
depleted, decreasing, increasing, stable,
impact relative to the size of the
population);
(5) Impacts on habitat affecting rates
of recruitment/survival; and
(6) The effectiveness of monitoring
and mitigation measures.
As described above and based on the
following factors, the specified activities
associated with the marine seismic
survey are not likely to cause PTS, or
other non-auditory injury, serious
injury, or death. The factors include:
(1) The likelihood that, given
sufficient notice through relatively slow
ship speed, marine mammals are
expected to move away from a noise
source that is annoying prior to its
becoming potentially injurious;
(2) The potential for temporary or
permanent hearing impairment is
relatively low and would likely be
avoided through the implementation of
the shut-down measures;
No injuries, serious injuries, or
mortalities are anticipated to occur as a
result of the NSF and ASC’s planned
low-energy marine seismic survey, and
none are proposed to be authorized by
NMFS. Table 5 of this document
outlines the number of requested Level
B harassment takes that are anticipated
as a result of these activities. Due to the
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
nature, degree, and context of Level B
(behavioral) harassment anticipated and
described (see ‘‘Potential Effects on
Marine Mammals’’ section above) in this
notice, the activity is not expected to
impact rates of annual recruitment or
survival for any affected species or
stock, particularly given NMFS’s and
the applicant’s proposal to implement
mitigation, monitoring, and reporting
measures to minimize impacts to marine
mammals. Additionally, the seismic
survey will not adversely impact marine
mammal habitat.
For the other marine mammal species
that may occur within the proposed
action area, there are no known
designated or important feeding and/or
reproductive areas. Many animals
perform vital functions, such as feeding,
resting, traveling, and socializing, on a
diel cycle (i.e., 24 hr cycle). Behavioral
reactions to noise exposure (such as
disruption of critical life functions,
displacement, or avoidance of important
habitat) are more likely to be significant
if they last more than one diel cycle or
recur on subsequent days (Southall et
al., 2007). Additionally, the seismic
survey will be increasing sound levels
in the marine environment in a
relatively small area surrounding the
vessel (compared to the range of the
animals), which is constantly travelling
over distances, and some animals may
only be exposed to and harassed by
sound for less than day.
Of the 14 marine mammal species
under NMFS jurisdiction that may or
are known to likely to occur in the study
area, five are listed as threatened or
endangered under the ESA: southern
right, humpback, sei, fin, blue, and
sperm whales. These species are also
considered depleted under the MMPA.
Of these ESA-listed species, incidental
take has been requested to be authorized
for humpback, sei, fin, blue, and sperm
whales. There is generally insufficient
data to determine population trends for
the other depleted species in the study
area. To protect these animals (and
other marine mammals in the study
area), NSF and ASC must cease or
reduce airgun operations if any marine
mammal enters designated zones. No
injury, serious injury, or mortality is
expected to occur and due to the nature,
degree, and context of the Level B
harassment anticipated, and the activity
is not expected to impact rates of
recruitment or survival.
As mentioned previously, NMFS
estimates that 14 species of marine
mammals under its jurisdiction could be
potentially affected by Level B
harassment over the course of the IHA.
The population estimates for the marine
mammal species that may be taken by
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Jkt 232001
Level B harassment were provided in
Table 4 of this document.
NMFS’s practice has been to apply the
160 dB re 1 mPa (rms) received level
threshold for underwater impulse sound
levels and the 120 dB re 1 mPa (rms)
received level threshold for icebreaking
activities to determine whether take by
Level B harassment occurs. Southall et
al. (2007) provide a severity scale for
ranking observed behavioral responses
of both free-ranging marine mammals
and laboratory subjects to various types
of anthropogenic sound (see Table 4 in
Southall et al. [2007]).
NMFS has preliminarily determined,
provided that the aforementioned
mitigation and monitoring measures are
implemented, the impact of conducting
a low-energy marine seismic survey in
the Dumont d’Urville Sea off the coast
of East Antarctica, February to March
2014, may result, at worst, in a
modification in behavior and/or lowlevel physiological effects (Level B
harassment) of certain species of marine
mammals.
While behavioral modifications,
including temporarily vacating the area
during the operation of the airgun(s),
may be made by these species to avoid
the resultant acoustic disturbance, the
availability of alternate areas within
these areas for species and the short and
sporadic duration of the research
activities, have led NMFS to
preliminary determine that the taking by
Level B harassment from the specified
activity will have a negligible impact on
the affected species in the specified
geographic region. NMFS believes that
the length of the seismic survey, the
requirement to implement mitigation
measures (e.g., shut-down of seismic
operations), and the inclusion of the
monitoring and reporting measures, will
reduce the amount and severity of the
potential impacts from the activity to
the degree that it will have a negligible
impact on the species or stocks in the
action area.
NMFS has preliminary determined,
provided that the aforementioned
mitigation and monitoring measures are
implemented, that the impact of
conducting a low-energy marine seismic
survey in the Dumont d’Urville Sea off
the coast of East Antarctica, January to
March 2014, may result, at worst, in a
temporary modification in behavior
and/or low-level physiological effects
(Level B harassment) of small numbers
of certain species of marine mammals.
See Table 5 for the requested authorized
take numbers of marine mammals.
Endangered Species Act
Of the species of marine mammals
that may occur in the proposed survey
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area, several are listed as endangered
under the ESA, including the
humpback, sei, fin, blue, and sperm
whales. NSF and ASC did not request
take of endangered Southern right
whales due to the low likelihood of
encountering this species during the
cruise. Under section 7 of the ESA, NSF,
on behalf of ASC and five other research
institutions, has initiated formal
consultation with the NMFS, Office of
Protected Resources, Endangered
Species Act Interagency Cooperation
Division, on this proposed seismic
survey. NMFS’s Office of Protected
Resources, Permits and Conservation
Division, has initiated formal
consultation under section 7 of the ESA
with NMFS’s Office of Protected
Resources, Endangered Species Act
Interagency Cooperation Division, to
obtain a Biological Opinion evaluating
the effects of issuing the IHA on
threatened and endangered marine
mammals and, if appropriate,
authorizing incidental take. NMFS will
conclude formal section 7 consultation
prior to making a determination on
whether or not to issue the IHA. If the
IHA is issued, NSF and ASC, in
addition to the mitigation and
monitoring requirements included in
the IHA, will be required to comply
with the Terms and Conditions of the
Incidental Take Statement
corresponding to NMFS’s Biological
Opinion issued to both NSF and ASC,
and NMFS’s Office of Protected
Resources.
National Environmental Policy Act
With NSF and ASC’s complete
application, NSF and ASC provided
NMFS a ‘‘Draft Initial Environmental
Evaluation/Environmental Assessment
to Conduct Marine-Based Studies of the
Totten Glacier System and Marine
Record of Cryosphere—Ocean
Dynamics,’’ (IEE/EA) prepared by
AECOM on behalf of NSF and ASC. The
IEE/EA analyzes the direct, indirect, and
cumulative environmental impacts of
the proposed specified activities on
marine mammals including those listed
as threatened or endangered under the
ESA. Prior to making a final decision on
the IHA application, NMFS will either
prepare an independent EA, or, after
review and evaluation of the NSF and
ASC IEE/EA for consistency with the
regulations published by the Council of
Environmental Quality (CEQ) and
NOAA Administrative Order 216–6,
Environmental Review Procedures for
Implementing the National
Environmental Policy Act, adopt the
NSF and ASC IEE/EA and make a
decision of whether or not to issue a
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3. Species Authorized and Level of
Takes
Proposed Authorization
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Finding of No Significant Impact
(FONSI).
(a) The incidental taking of marine
mammals, by Level B harassment only,
is limited to the following species in the
waters of the Southern Ocean off the
coast of East Antarctica:
(i) Mysticetes—see Table 2 (attached)
for authorized species and take
numbers.
(ii) Odontocetes—see Table 2
(attached) for authorized species and
take numbers.
(iii) Pinnipeds—see Table 2 (attached)
for authorized species and take
numbers.
(iv) If any marine mammal species are
encountered during seismic activities
that are not listed in Table 2 (attached)
for authorized taking and are likely to be
exposed to sound pressure levels (SPLs)
greater than or equal to 160 dB re 1 mPa
(rms) for seismic airgun operations or
greater than or equal to 120 dB re 1 mPa
(rms) for icebreaking activities, then the
Holder of this Authorization must alter
speed or course or shut-down the
airguns to avoid take.
(b) The taking by injury (Level A
harassment), serious injury, or death of
any of the species listed in Condition
3(a) above or the taking of any kind of
any other species of marine mammal is
prohibited and may result in the
modification, suspension or revocation
of this Authorization.
4. The methods authorized for taking
by Level B harassment are limited to the
following acoustic sources without an
amendment to this Authorization:
(a) A two Generator Injector (GI)
airgun array (each with a discharge
volume of 45 cubic inches [in3] or 105
in3) with a total volume of 90 in3 or 210
in3 (or smaller);
(b) A multi-beam echosounder;
(c) A single-beam echosounder;
(d) An acoustic Doppler current
profiler;
(e) An acoustic locator;
(f) A sub-bottom profiler; and
(g) Icebreaking.
5. The taking of any marine mammal
in a manner prohibited under this
Authorization must be reported
immediately to the Office of Protected
Resources, National Marine Fisheries
Service (NMFS), at 301–427–8401.
As a result of these preliminary
determinations, NMFS propose to issue
an IHA to NSF and ASC for conducting
the low-energy seismic survey in the
tropical western Pacific Ocean,
provided the previously mentioned
mitigation, monitoring, and reporting
requirements are incorporated. The
proposed IHA language is provided
below:
National Science Foundation,
Division of Polar Programs, 4201 Wilson
Boulevard, Arlington, Virginia 22230
and Antarctic Support Contract, 7400
South Tucson Way, Centennial,
Colorado 80112, is hereby authorized
under section 101(a)(5)(D) of the Marine
Mammal Protection Act (MMPA) (16
U.S.C. 1371(a)(5)(D)), to harass small
numbers of marine mammals incidental
to a low-energy marine geophysical
(seismic) survey conducted by the RVIB
Nathaniel B. Palmer (Palmer) in the
Dumont d’Urville Sea, Antarctica,
January to March 2014:
1. This Authorization is valid from
January 29 through April 27, 2014.
2. This Authorization is valid only for
the Palmer’s activities associated with
low-energy seismic survey operations
that shall occur in the following
specified geographic area:
In selected regions of the Dumont
d’Urville Sea in the Southern Ocean off
the coast of East Antarctica and focus on
the Totten Glacier and Moscow
University Ice Shelf, located on the
Sabrina Coast, from greater than
approximately 64° South and between
approximately 95 to 135° East, and the
Mertz Glacier and Cook Ice Shelf
systems located on the George V and
Oates Coast, from greater than
approximately 65° South and between
approximately 140 to 165° East. The
study sites are characterized by heavy
ice cover, with a seasonal break-up in
the ice that structures biological
patterns. The studies may occur in both
areas, or entirely in one or the other,
depending on ice conditions. Water
depths in the survey area generally
range from approximately 100 to 1,000
m, and possibly exceeding 1,000 m in
some areas. The low-energy seismic
survey will be conducted in
International Waters (i.e., high seas), as
specified in NSF and ASC’s Incidental
Harassment Authorization application
and the associated NSF and ASC Initial
Environmental Evaluation/
Environmental Assessment (IEE/EA).
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6. Mitigation and Monitoring
Requirements
The Holder of this Authorization is
required to implement the following
mitigation and monitoring requirements
when conducting the specified activities
to achieve the least practicable adverse
impact on affected marine mammal
species or stocks:
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495
(a) Utilize one, NMFS-qualified,
vessel-based Protected Species Observer
(PSO) to visually watch for and monitor
marine mammals near the seismic
source vessel during daytime airgun
operations (from nautical twilight-dawn
to nautical twilight-dusk) and before
and during ramp-ups of airguns day or
night. The Palmer’s vessel crew shall
also assist in detecting marine
mammals, when practicable. PSOs shall
have access to reticle binoculars (7 × 50
Fujinon). PSO shifts shall last no longer
than 4 hours at a time. PSOs shall also
make observations during daytime
periods when the seismic airguns are
not operating for comparison of animal
abundance and behavior, when feasible.
(b) PSOs shall conduct monitoring
while the airgun array and streamer are
being deployed or recovered from the
water.
(c) Record the following information
when a marine mammal is sighted:
(i) Species, group size, age/size/sex
categories (if determinable), behavior
when first sighted and after initial
sighting, heading (if consistent), bearing
and distance from seismic vessel,
sighting cue, apparent reaction to the
airguns or vessel (e.g., none, avoidance,
approach, paralleling, etc., and
including responses to ramp-up), and
behavioral pace; and
(ii) Time, location, heading, speed,
activity of the vessel (including number
of airguns operating and whether in
state of ramp-up or shut-down),
Beaufort sea state and wind force,
visibility, and sun glare; and
(iii) The data listed under Condition
6(c)(ii) shall also be recorded at the start
and end of each observation watch and
during a watch whenever there is a
change in one or more of the variables.
(d) Visually observe the entire extent
of the exclusion zone (180 dB re 1 mPa
[rms] for cetaceans and 190 dB re 1 mPa
[rms] for pinnipeds; see Table 2 [above]
for distances) using NMFS-qualified
PSOs, for at least 30 minutes prior to
starting the airgun array (day or night).
If the PSO finds a marine mammal
within the exclusion zone, NSF and
ASC must delay the seismic survey until
the marine mammal(s) has left the area.
If the PSO sees a marine mammal that
surfaces, then dives below the surface,
the PSO shall wait 30 minutes. If the
PSO sees no marine mammals during
that time, they should assume that the
animal has moved beyond the exclusion
zone. If for any reason the entire radius
cannot be seen for the entire 30 minutes
(i.e., rough seas, fog, darkness), or if
marine mammals are near, approaching,
or in the exclusion zone, the airguns
may not be ramped-up. If one airgun is
already running at a source level of at
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Federal Register / Vol. 79, No. 2 / Friday, January 3, 2014 / Notices
least 180 dB re 1 mPa (rms), NSF and
ASC may start the second airgun
without observing the entire exclusion
zone for 30 minutes prior, provided no
marine mammals are known to be near
the exclusion zone (in accordance with
Condition 6[f] below).
(e) Establish a 180 dB re 1 mPa (rms)
exclusion zone for cetaceans and a 190
dB re 1 mPa (rms) exclusion zone for
pinnipeds before the two GI airgun array
(90 or 210 in3 total volume) is in
operation. See Table 2 (above) for
distances and exclusion zones.
(f) Implement a ‘‘ramp-up’’ procedure
when starting up at the beginning of
seismic operations or anytime after the
entire array has been shut-down for
more than 15 minutes, which means
starting with a single GI airgun and
adding a second GI airgun after five
minutes. During ramp-up, the PSOs
shall monitor the exclusion zone, and if
marine mammals are sighted, a shutdown shall be implemented as though
the full array (both GI airguns) were
operational. Therefore, initiation of
ramp-up procedures from shut-down
requires that the PSOs be able to view
the full exclusion zone as described in
Condition 6(d) (above).
(g) Alter speed or course during
seismic operations if a marine mammal,
based on its position and relative
motion, appears likely to enter the
relevant exclusion zone. If speed or
course alteration is not safe or
practicable, or if after alteration the
marine mammal still appears likely to
enter the exclusion zone, further
mitigation measures, such as a shutdown, shall be taken.
(h) Shut-down the airgun(s) if a
marine mammal is detected within,
approaches, or enters the relevant
exclusion zone (as defined in Table 2,
above). A shut-down means all
operating airguns are shut-down (i.e.,
turned off).
(i) Following a shut-down, the airgun
activity shall not resume until the PSO
has visually observed the marine
mammal(s) exiting the exclusion zone
and is not likely to return, or has not
been seen within the exclusion zone for
15 minutes for species with shorter dive
durations (small odontocetes and
pinnipeds) or 30 minutes for species
with longer dive durations (mysticetes
and large odontocetes, including sperm,
killer, and beaked whales).
(j) Following a shut-down and
subsequent animal departure, airgun
operations may resume following rampup procedures described in Condition
6(f).
(k) Marine seismic surveys may
continue into night and low-light hours
if such segment(s) of the survey is
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initiated when the entire relevant
exclusion zones are visible and can be
effectively monitored.
(l) No initiation of airgun array
operations is permitted from a shutdown position at night or during lowlight hours (such as in dense fog or
heavy rain) when the entire relevant
exclusion zone cannot be effectively
monitored by the PSO(s) on duty.
7. Reporting Requirements
The Holder of this Authorization is
required to:
(a) Submit a draft report on all
activities and monitoring results to the
Office of Protected Resources, NMFS,
within 90 days of the completion of the
Palmer’s Dumont d’Urville Sea off the
coast of East Antarctica cruise. This
report must contain and summarize the
following information:
(i) Dates, times, locations, heading,
speed, weather, sea conditions
(including Beaufort sea state and wind
force), and associated activities during
all seismic operations and marine
mammal sightings;
(ii) Species, number, location,
distance from the vessel, and behavior
of any marine mammals, as well as
associated seismic activity (e.g., number
of shut-downs), observed throughout all
monitoring activities.
(iii) An estimate of the number (by
species) of marine mammals that: (A)
Are known to have been exposed to the
seismic activity (based on visual
observation) at received levels greater
than or equal to 120 dB re 1 mPa (rms)
(for icebreaking activities), greater than
or equal to 160 dB re 1 mPa (rms) (for
seismic airgun operations), and/or 180
dB re 1 mPa (rms) for cetaceans and 190
dB re 1 mPa (rms) for pinnipeds with a
discussion of any specific behaviors
those individuals exhibited; and (B)
may have been exposed (based on
modeled values for the two GI airgun
array) to the seismic activity at received
levels greater than or equal to 120 dB re
1 mPa (rms) (for icebreaking activities),
greater than or equal to 160 dB re 1 mPa
(rms) (for seismic airgun operations),
and/or 180 dB re 1 mPa (rms) for
cetaceans and 190 dB re 1 mPa (rms) for
pinnipeds with a discussion of the
nature of the probable consequences of
that exposure on the individuals that
have been exposed.
(iv) A description of the
implementation and effectiveness of the:
(A) Terms and Conditions of the
Biological Opinion’s Incidental Take
Statement (ITS) (attached); and (B)
mitigation measures of the Incidental
Harassment Authorization. For the
Biological Opinion, the report shall
confirm the implementation of each
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Term and Condition, as well as any
conservation recommendations, and
describe their effectiveness, for
minimizing the adverse effects of the
action on Endangered Species Act-listed
marine mammals.
(b) Submit a final report to the Chief,
Permits and Conservation Division,
Office of Protected Resources, NMFS,
within 30 days after receiving comments
from NMFS on the draft report. If NMFS
decides that the draft report needs no
comments, the draft report shall be
considered to be the final report.
8. In the unanticipated event that the
specified activity clearly causes the take
of a marine mammal in a manner
prohibited by this Authorization, such
as an injury (Level A harassment),
serious injury or mortality (e.g., shipstrike, gear interaction, and/or
entanglement), NSF and ASC shall
immediately cease the specified
activities and immediately report the
incident to the Chief of the Permits and
Conservation Division, Office of
Protected Resources, NMFS, at 301–
427–8401 and/or by email to
Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report
must include the following information:
(a) Time, date, and location (latitude/
longitude) of the incident; the name and
type of vessel involved; the vessel’s
speed during and leading up to the
incident; description of the incident;
status of all sound source use in the 24
hours preceding the incident; water
depth; environmental conditions (e.g.,
wind speed and direction, Beaufort sea
state, cloud cover, and visibility);
description of marine mammal
observations in the 24 hours preceding
the incident; species identification or
description of the animal(s) involved;
the fate of the animal(s); and
photographs or video footage of the
animal (if equipment is available).
Activities shall not resume until
NMFS is able to review the
circumstances of the prohibited take.
NMFS shall work with NSF and ASC to
determine what is necessary to
minimize the likelihood of further
prohibited take and ensure MMPA
compliance. NSF and ASC may not
resume their activities until notified by
NMFS via letter, email, or telephone.
In the event that NSF and ASC
discovers an injured or dead marine
mammal, and the lead PSO determines
that the cause of the injury or death is
unknown and the death is relatively
recent (i.e., in less than a moderate state
of decomposition as described in the
next paragraph), NSF and ASC will
immediately report the incident to the
Chief of the Permits and Conservation
Division, Office of Protected Resources,
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NMFS, at 301–427–8401, and/or by
email to Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report
must include the same information
identified in Condition 8(a) above.
Activities may continue while NMFS
reviews the circumstances of the
incident. NMFS will work with NSF
and ASC to determine whether
modifications in the activities are
appropriate.
In the event that NSF and ASC
discovers an injured or dead marine
mammal, and the lead PSO determines
that the injury or death is not associated
with or related to the activities
authorized in Condition 2 of this
Authorization (e.g., previously wounded
animal, carcass with moderate to
advanced decomposition, or scavenger
damage), NSF and ASC shall report the
incident to the Chief of the Permits and
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Conservation Division, Office of
Protected Resources, NMFS, at 301–
427–8401, and/or by email to
Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov, within 24
hours of the discovery. NSF and ASC
shall provide photographs or video
footage (if available) or other
documentation of the stranded animal
sighting to NMFS and the Marine
Mammal Stranding Network. Activities
may continue while NMFS reviews the
circumstances of the incident.
9. NSF and ASC is required to comply
with the Terms and Conditions of the
ITS corresponding to NMFS’s Biological
Opinion issued to both NSF, ASC, and
NMFS’s Office of Protected Resources
(attached).
10. A copy of this Authorization and
the ITS must be in the possession of all
contractors and PSOs operating under
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497
the authority of this Incidental
Harassment Authorization.
Information Solicited
NMFS requests interested persons to
submit comments and information
concerning this proposed project and
NMFS’s preliminary determination of
issuing an IHA (see ADDRESSES).
Concurrent with the publication of this
notice in the Federal Register, NMFS is
forwarding copies of this application to
the Marine Mammal Commission and
its Committee of Scientific Advisors.
Dated: December 30, 2013.
P. Michael Payne,
Chief, Permits and Conservation Division,
Office of Protected Resources, National
Marine Fisheries Service.
[FR Doc. 2013–31471 Filed 12–31–13; 8:45 am]
BILLING CODE 3510–22–P
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Agencies
[Federal Register Volume 79, Number 2 (Friday, January 3, 2014)]
[Notices]
[Pages 463-497]
From the Federal Register Online via the Government Printing Office [www.gpo.gov]
[FR Doc No: 2013-31471]
[[Page 463]]
Vol. 79
Friday,
No. 2
January 3, 2014
Part III
Department of Commerce
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National Oceanic and Atmospheric Administration
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Takes of Marine Mammals Incidental to Specified Activities; Low-Energy
Marine Geophysical Survey in the Dumont d'Urville Sea Off the Coast of
East Antarctica, January to March 2013; Notice
Federal Register / Vol. 79 , No. 2 / Friday, January 3, 2014 /
Notices
[[Page 464]]
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DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric Administration
RIN 0648-XC779
Takes of Marine Mammals Incidental to Specified Activities; Low-
Energy Marine Geophysical Survey in the Dumont d'Urville Sea Off the
Coast of East Antarctica, January to March 2013
AGENCY: National Marine Fisheries Service (NMFS), National Oceanic and
Atmospheric Administration (NOAA), Commerce.
ACTION: Notice; proposed Incidental Harassment Authorization; request
for comments.
-----------------------------------------------------------------------
SUMMARY: NMFS has received an application from the National Science
Foundation (NSF) Division of Polar Programs, and Antarctic Support
Contract (ASC) on behalf of five research institutions: Colgate
University, Columbia University, Texas A&M Research Foundation,
University of South Florida, and University of Texas at Austin, for an
Incidental Harassment Authorization (IHA) to take marine mammals, by
harassment, incidental to conducting a low-energy marine geophysical
(seismic) survey in the Dumont d'Urville Sea off the coast of East
Antarctica, January to March 2014. Pursuant to the Marine Mammal
Protection Act (MMPA), NMFS is requesting comments on its proposal to
issue an IHA to NSF to incidentally harass, by Level B harassment only,
14 species of marine mammals during the specified activity.
DATES: Comments and information must be received no later than February
3, 2014.
ADDRESSES: Comments on the application should be addressed to P.
Michael Payne, Chief, Permits and Conservation Division, Office of
Protected Resources, National Marine Fisheries Service, 1315 East-West
Highway, Silver Spring, MD 20910. The mailbox address for providing
email comments is ITP.Goldstein@noaa.gov. NMFS is not responsible for
email comments sent to addresses other than the one provided here.
Comments sent via email, including all attachments, must not exceed a
10-megabyte file size.
All comments received are a part of the public record and will
generally be posted to https://www.nmfs.noaa.gov/pr/permits/incidental.htm#applications without change. All Personal Identifying
Information (for example, name, address, etc.) voluntarily submitted by
the commenter may be publicly accessible. Do not submit confidential
business information or otherwise sensitive or protected information.
A copy of the application containing a list of the references used
in this document may be obtained by writing to the above address,
telephoning the contact listed here (see FOR FURTHER INFORMATION
CONTACT) or visiting the internet at: https://www.nmfs.noaa.gov/pr/permits/incidental.htm#applications.
NSF and ASC have provided a ``Draft Initial Environmental
Evaluation/Environmental Assessment to Conduct a Marine-Based Studies
of the Totten Glacier System and Marine Record of Cryosphere--Ocean
Dynamics'' (IEE/EA), prepared by AECOM, on behalf of NSF and ASC, which
is also available at the same Internet address. Documents cited in this
notice may be viewed, by appointment, during regular business hours, at
the aforementioned address.
FOR FURTHER INFORMATION CONTACT: Howard Goldstein or Jolie Harrison,
Office of Protected Resources, NMFS, 301-427-8401.
SUPPLEMENTARY INFORMATION:
Background
Section 101(a)(5)(D) of the MMPA, as amended (16 U.S.C. 1371
(a)(5)(D)), directs the Secretary of Commerce (Secretary) to authorize,
upon request, the incidental, but not intentional, taking of small
numbers of marine mammals of a species or population stock, by United
States citizens who engage in a specified activity (other than
commercial fishing) within a specified geographical region if certain
findings are made and, if the taking is limited to harassment, a notice
of a proposed authorization is provided to the public for review.
Authorization for the incidental taking of small numbers of marine
mammals shall be granted if NMFS finds that the taking will have a
negligible impact on the species or stock(s), and will not have an
unmitigable adverse impact on the availability of the species or
stock(s) for subsistence uses (where relevant). The authorization must
set forth the permissible methods of taking, other means of effecting
the least practicable adverse impact on the species or stock and its
habitat, and requirements pertaining to the mitigation, monitoring and
reporting of such takings. NMFS has defined ``negligible impact'' in 50
CFR 216.103 as ``. . . an impact resulting from the specified activity
that cannot be reasonably expected to, and is not reasonably likely to,
adversely affect the species or stock through effects on annual rates
of recruitment or survival.''
Section 101(a)(5)(D) of the MMPA established an expedited process
by which citizens of the United States can apply for an authorization
to incidentally take small numbers of marine mammals by harassment.
Section 101(a)(5)(D) of the MMPA establishes a 45-day time limit for
NMFS's review of an application followed by a 30-day public notice and
comment period on any proposed authorizations for the incidental
harassment of small numbers of marine mammals. Within 45 days of the
close of the public comment period, NMFS must either issue or deny the
authorization.
Except with respect to certain activities not pertinent here, the
MMPA defines ``harassment'' as: Any act of pursuit, torment, or
annoyance which (i) has the potential to injure a marine mammal or
marine mammal stock in the wild [Level A harassment]; or (ii) has the
potential to disturb a marine mammal or marine mammal stock in the wild
by causing disruption of behavioral patterns, including, but not
limited to, migration, breathing, nursing, breeding, feeding, or
sheltering [Level B harassment].
Summary of Request
On July 3, 2013, NMFS received an application from the NSF and ASC
requesting that NMFS issue an IHA for the take, by Level B harassment
only, of small numbers of marine mammals incidental to conducting a
low-energy marine seismic survey in International Waters (i.e., high
seas) and in the Southern Ocean off the coast of East Antarctica during
January to March 2014. We received an addendum to the application from
the NSF and ASC on December 18, 2013 which reflected updates to
incidental take requests for marine mammals related to icebreaking
activities.
The research would be conducted by five research institutions:
Colgate University, Columbia University, Texas A&M Research Foundation,
University of South Florida, and University of Texas at Austin. The NSF
and ASC plans to use one source vessel, the R/VIB Nathaniel B. Palmer
(Palmer), and a seismic airgun array to collect seismic data in the
Southern Ocean. The vessel would be operated by ASC, which operates the
United States Antarctic Program under contract to the NSF. In support
of the United States Antarctic Program, the NSF and ASC plans to use
conventional low-energy, seismic methodology to perform marine-based
studies in the Dumont d'Urville Sea to include evaluation of
geophysical and physical oceanographic features in two
[[Page 465]]
areas along the coast of East Antarctica (see Figures 1, 2, and 3 of
the IHA application). The primary area proposed for the study is the
Totten Glacier system (preferred study area) including the Moscow
University Ice Shelf along the Sabrina Coast, and a secondary area, the
Mertz Glacier and Cook Ice Shelf, along the Oates Coast. In addition to
the proposed operations of the seismic airgun array and hydrophone
streamer, NSF and ASC intend to operate a single-beam echosounder,
multi-beam echosounder, acoustic Doppler current profiler (ADCP), and
sub-bottom profiler continuously throughout the survey.
Acoustic stimuli (i.e., increased underwater sound) generated
during the operation of the seismic airgun array and from icebreaking
activities may have the potential to cause a behavioral disturbance for
marine mammals in the survey area. This is the principal means of
marine mammal taking associated with these activities, and NSF and ASC
has requested an authorization to take 14 species of marine mammals by
Level B harassment. Take is not expected to result from the use of the
single-beam echosounder, multi-beam echosounder, ADCP, acoustic
locator, and sub-bottom profiler, as the brief exposure of marine
mammals to one pulse, or small numbers of signals, in this particular
case is not likely to result in the harassment of marine mammals. Also,
NMFS does not expect take to result from collision with the source
vessel because it is a single vessel moving at a relatively slow,
constant cruise speed of 5 knots [kts]; 9.3 kilometers per hour [km/
hr]; 5.8 miles per hour [mph]) during seismic acquisition within the
survey, for a relatively short period of time (approximately 45
operational days). It is likely that any marine mammal would be able to
avoid the vessel.
Description of the Proposed Specified Activity
NSF and ASC propose to conduct a low-energy seismic survey in the
Dumont d'Urville Sea in the Southern Ocean off the coast of East
Antarctica from January to March 2014. In addition to the low-energy
seismic survey, scientific activities would include conducting a
bathymetric profile survey of the seafloor using transducer based
instruments such as a multi-beam echosounder and sub-bottom profiler;
conducting magnetometry and imaging surveys using an underwater camera
assembly; collecting sediment cores and dredge sampling; and collecting
water samples and conductivity (salinity), temperature, depth (CTD) and
current data through the deployment and recovery of short-term (in
place for approximately one month) and long-term (in place for
approximately one year) instrumentation moorings, CTD equipment casts,
and the use of transducer-based ADCP instruments. Sea ice conditions
will dictate areas where the ship and airguns can operate. Due to
dynamic ice conditions, which cannot be predicted on a local scale, it
is not possible to develop tracklines a priori. The seismic survey
would be conducted in one or both of the two study areas depending on
the sea ice conditions; however, the preferred study area is the Totten
Glacier region (see Figure 2 of the IHA application). Water depths in
the survey area range from 100 to 1,000 meters (m) (328.1 to 3,280.1
feet [ft]), and possibly exceeding 1,000 m in some areas. The seismic
surveys are scheduled to occur for a total of less than or equal to 300
hours at one or both of the two study areas for approximately 45
operational days in January to March 2014. The operation hours and
survey length would include equipment testing, ramp-up, line changes,
and repeat coverage. The long transit time between port and the study
site constrains how long the ship can be in the study area and
effectively limits the maximum amount of time the airguns can operate.
Some minor deviation from these dates would be possible, depending on
logistics and weather.
The proposed survey of Totten Glacier and Moscow University Ice
Shelf along the Sabrina Coast continental shelf is designed to address
several critical questions. The Totten Glacier system, which drains
one-eighth of the East Antarctic Ice Sheet and contains more ice volume
than the entire West Antarctic Ice Sheet, remains the single largest
and least understood glacial system which possesses a potentially
unsteady dynamic. If it were to melt, sea-level would rise by more than
5 m (16.4 ft) worldwide. The proposed marine studies would help to
understand both the dynamics and the controls of the Totten Glacier
system, and to resolve ambiguity in large ice mass dynamic behavior.
This research would be accomplished via the collection of
glaciological, geological, and physical oceanographic data. In order to
place the modern system, as well as more recent changes to the system,
into a longer-term perspective, researchers would collect and interpret
marine geologic, geochemical, and geophysical records of the longer
term behavior and response of this system.
The proposed research would complement fieldwork studying other
Antarctic ice shelves oceanographic studies near the Antarctic
Peninsula, and ongoing development of ice sheet and other ocean models.
It would facilitate learning at sea and ashore by students, help to
fill important spatial and temporal gaps in a sparsely sampled region
of coastal Antarctica, and communicate its findings via publications
and outreach. Obtaining records of currents and oceanographic
properties in this region are consistent with the objectives of the
Southern Ocean Observing System for climate change. The work would
enhance general understanding of air-sea-ice interactions, ocean
circulation, ice shelf sensitivity to climate change, and the present
and future roles of East Antarctic Ice Sheet on sea level.
The Principal Investigators are Dr. Amy Leventer of Colgate
University, Dr. Donald Blankenship and Dr. Sean Gulick of the
University of Texas at Austin, Dr. Eugene Domack of the University of
South Florida, Mr. Bruce Huber of Columbia University, and Dr.
Alejandro Orsi of Texas A&M Research Foundation.
The procedures to be used for the surveys would be similar to those
used during previous low-energy seismic surveys by NSF and would use
conventional seismic methodology. The proposed survey will involve one
source vessel, the R/V Nathaniel B. Palmer (Palmer). NSF and ASC will
deploy two (each with a discharge volume of 45 cubic inch [in\3\] with
a total volume of 90 in\3\ or each with a discharge volume of 105 in\3\
with a total volume of 210 in\3\) Sercel Generator Injector (GI) airgun
array as an energy source at a tow depth of up to 3 m (9.8 ft) below
the surface (more information on the airguns can be found in Appendix B
of the IHA application). The receiving system will consist of one 100 m
(328.1 ft) long, 24-channel, solid-state hydrophone streamer towed
behind the vessel. As the GI airguns are towed along the survey lines,
the hydrophone streamer will receive the returning acoustic signals and
transfer the data to the onboard processing system. All planned seismic
data acquisition activities will be conducted by technicians provided
by NSF and ASC with onboard assistance by the scientists who have
proposed the study. The vessel will be self-contained, and the crew
will live aboard the vessel for the entire cruise.
The planned seismic survey (e.g., equipment testing, start-up, line
changes, repeat coverage of any areas, and equipment recovery) will
consist of approximately 2,800 kilometer (km) (1,511.9 nautical miles
[nmi]) of transect lines (including turns) in the survey area in the
Dumont d'Urville Sea of the
[[Page 466]]
Southern Ocean (see Figures 1, 2, and 3 of the IHA application). In
addition to the operation of the airgun array, a single-beam and multi-
beam echosounder, ADCP, and a sub-bottom profiler will also likely be
operated from the Palmer continuously throughout the cruise between the
first and last survey sites. There will be additional seismic
operations associated with equipment testing, ramp-up, and possible
line changes or repeat coverage of any areas where initial data quality
is sub-standard. In NSF and ASC's estimated take calculations, 25% has
been added for those additional operations.
Table 1--Proposed Low-Energy Seismic Survey Activities in the Dumont d'Urville Sea Off the Coast of East
Antarctica
----------------------------------------------------------------------------------------------------------------
Cumulative
Survey length (km) duration (hr) Airgun array total Time between airgun Streamer length (m)
\1\ volume shots (distance)
----------------------------------------------------------------------------------------------------------------
2,800 (1,511.9 nmi)............. <=300 2 x 45 in\3\ (2 x 5 seconds (12.5 m 100 (328.1 ft).
737 cm\3\) or or 41 ft).
2 x 105 in\3\ (2 x
1,720 cm\3\).
----------------------------------------------------------------------------------------------------------------
\1\ Airgun operations are planned for no more than 16 continuous hours at a time.
Vessel Specifications
The Palmer, a research vessel owned by Edison Chouest Offshore,
Inc. and operated by NSF and ACS (under a long-term charter with Edison
Chouest Offshore, Inc.), will tow the two GI airgun array, as well as
the hydrophone streamer. When the Palmer is towing the airgun array and
the relatively short hydrophone streamer, the turning rate of the
vessel while the gear is deployed is much higher than the limit of 5
degrees per a minute for a seismic vessel towing a streamer of more
typical length (much greater than 1 km [0.5 nmi]), which is
approximately 20 degrees. Thus, the maneuverability of the vessel is
not limited much during operations with the streamer.
The U.S.-flagged vessel has a length of 94 m (308.5 ft); a beam of
18.3 m (60 ft); a maximum draft of 6.8 m (22.5 ft); and a gross tonnage
of 6,174. The ship is powered by four Caterpillar 3608 diesel engines
(3,300 brake horsepower [hp] at 900 rotations per minute [rpm]) and a
1,400 hp flush-mounted, water jet azimuthing bowthruster. Electrical
power is provided by four Catepillar 3512, 1,050 kiloWatt (kW) diesel
generators. The Palmer's operation speed during seismic acquisition is
typically approximately 9.3 km/hr (5 kts) (varying between 7.4 to 11.1
km/hr [4 to 6 kts]). When not towing seismic survey gear, the Palmer
typically cruises at 18.7 km/hr (10.1 kts) and has a maximum speed of
26.9 km/hr (14.5 kts). The Palmer has an operating range of
approximately 27,780 km (15,000 nmi) (the distance the vessel can
travel without refueling), which is approximately 70 to 75 days. The
vessel can accommodate 37 scientists and 22 crew members.
The vessel also has two locations as likely observation stations
from which Protected Species Observers (PSO) will watch for marine
mammals before and during the proposed airgun operations on the Palmer.
Observing stations will be at the bridge level with PSO's eye level
approximately 16.5 m (54.1 ft) above sea level with an approximately
270[deg] view around the vessel, and an aloft observation tower that is
approximately 24.4 m (80.1 ft) above sea level that is protected from
the weather and has an approximately 360[deg] view around the vessel.
More details of the Palmer can be found in the IHA application and
online at: https://www.nsf.gov/geo/plr/support/nathpalm.jsp and https://www.usap.gov/vesselScienceAndOperations/contentHandler.cfm?id=1561.
Acoustic Source Specifications
Seismic Airguns
The Palmer will deploy an airgun array, consisting of two 45 in\3\
or two 105 in\3\ GI airguns as the primary energy source and a 100 m
streamer containing hydrophones. The airgun array will have a supply
firing pressure of 2,000 pounds per square inch (psi) and 2,200 psi
when at high pressure stand-by (i.e., shut-down). The regulator is
adjusted to ensure that the maximum pressure to the GI airguns is 2,000
psi, but there are times when the GI airguns may be operated at
pressures as low as 1,750 to 1,800 psi Seismic pulses for the GI
airguns will be emitted at intervals of approximately 5 seconds. At
speeds of approximately 9.3 km/hr, the shot intervals correspond to
spacing of approximately will be 12.5 m (41 ft) during the study. There
would be approximately 720 shots per hour. During firing, a brief
(approximately 0.03 second) pulse sound is emitted; the airguns will be
silent during the intervening periods. The dominant frequency
components range from two to 188 Hertz (Hz).
The GI airguns would be used in harmonic mode, that is, the volume
of the injector chamber (I) of each GI airgun is equal to that of its
generator chamber (G): 45 in\3\ and 105 in\3\ for each airgun array.
Each airgun would be initially configured to a displacement volume of
45 in\3\ for the generator and injector. The generator chamber of each
GI airgun in the primary source, the one responsible for introducing
the sound pulse into the ocean, is 45 in\3\. The injector chamber
injects air into the previously-generated bubble to maintain its shape,
and does not introduce more sound into the water. The airguns would
fire the compressed air volume in unison in a harmonic mode. In
harmonic mode, the injector volume is designed to destructively
interfere with the reverberations of the generator (source component).
Firing the airguns in harmonic mode maximizes resolution in the data
and minimizes any excess noise in the water column or data caused by
the reverberations (or bubble pulses). The two GI airguns will be
spaced approximately 3 or 6 m (9.8 or 19.7 ft) apart, side-by-side,
between 15 and 40 m (49.2 and 131.2 ft) behind the Palmer, at a depth
of up to 3 m during the surveys. If needed to improve penetration of
the strata, the two airguns may be reconfigured to a displacement
volume of 105 in\3\ each and would still be considered a low-energy
acoustic source as defined in the NSF/USGS PEIS. Therefore, there are
three possible two airgun array configurations: Two 45/45 in\3\ airguns
separated by 3 m, two 45/45 in\3\ airguns separated by 6 m, and two
105/105 in\3\ airguns separated by 3 m. The two 45/45 in\3\ airguns
separated by 3 m layout is preferred, the two 45/45 in\3\ separated by
6 m layout would be used in the event the middle of the three 45/45
in\3\ airgun fails, and the two 105/105 in\3\ airguns separated by 3 m
would be used only if additional penetration is needed. To summarize,
two strings of GI airguns would be available: (1) Three 45/45 in\3\
airguns on a single string where one of these is used as a ``hot
spare'' in the event of
[[Page 467]]
failure of one of the other two airguns, these three GI airguns are
separated by 3 m; and (2) two 105/105 in\3\ airguns on a second string
without a ``hot spare.'' The total effective volume will be 90 or 210
in\3\. The two strings would be spaced 14 m (45.9 ft) apart, on either
side of the midline of the vessel, however, only one string at a time
would be used.
The Nucleus modeling software used at Lamont-Doherty Earth
Observatory of Columbia University (L-DEO) does not include GI airguns
as part of its airgun library, however signatures and mitigation models
have been obtained for two 45 in\3\ G airguns at 2 m tow depth and two
105 in\3\ G airguns at 3 m tow depth that are close approximations. For
the two 45 in\3\ airgun array, the source output (downward) is 230.6 dB
re: 1 [mu]Pam for 0-to-peak and 235.9 dB re: 1 [mu]Pam for peak-to-
peak. For the two 105 in\3\ airgun array, the source output (downward)
is 234.4 dB re: 1 [mu]Pam 0-to-peak and 239.8 dB re: 1 [mu]Pam for
peak-to-peak. These numbers were determined using the aforementioned G-
airgun approximation to the GI airgun and using signatures filtered
with DFS V out-256 Hz 72 dB/octave. The dominant frequency range would
be 20 to 160 Hz for a pair of GI airguns towed at 3 m depth and 35 to
230 Hz for a pair of GI airguns towed at 2 m depth.
During the low-energy seismic survey, the vessel would attempt to
maintain a constant cruise speed of approximately 5 knots. The airguns
would operate continuously for no more than 16 hours at a time and
duration of continuous operation is dependent on ice concentration. The
cumulative duration of the airgun operations will not exceed 200 hrs.
The relatively short, 24-channel hydrophone streamer would provide
operational flexibility to allow the seismic survey to proceed along
the designated cruise track with minimal interruption due to variable
sea ice conditions. The design of the seismic equipment is to achieve
high-resolution images of the glacial marine sequence stratigraphy with
the ability to correlate to the ultra-high frequency sub-bottom
profiling data and provide cross-sectional views to pair with the
seafloor bathymetry. The cruise path would be designated once in the
study area and would take care to avoid heavy ice conditions such as
icebergs or dense areas of pack ice that could potentially damage the
airguns or streamer and minimize proximity to potential marine
receptors.
Weather conditions that could affect the movement of sea ice and
hinder the hydrophone streamer would be closely monitored, as well as
conditions that could limit visibility. If situations are encountered
which pose a risk to the equipment, impede data collection, or require
the vessel to stop forward progress, the seismic survey equipment would
be shut-down and retrieved until conditions improve. In general, the
hydrophone streamer and sources could be retrieved in less than 30
minutes.
Metrics Used in This Document
This section includes a brief explanation of the sound measurements
frequently used in the discussions of acoustic effects in this
document. Sound pressure is the sound force per unit area, and is
usually measured in micropascals ([mu]Pa), where 1 pascal (Pa) is the
pressure resulting from a force of one newton exerted over an area of
one square meter. Sound pressure level (SPL) is expressed as the ratio
of a measured sound pressure and a reference level. The commonly used
reference pressure level in underwater acoustics is 1 [mu]Pa, and the
units for SPLs are dB re: 1 [mu]Pa. SPL (in decibels [dB]) = 20 log
(pressure/reference pressure).
SPL is an instantaneous measurement and can be expressed as the
peak, the peak-to-peak (p-p), or the root mean square (rms). Root mean
square, which is the square root of the arithmetic average of the
squared instantaneous pressure values, is typically used in discussions
of the effects of sounds on vertebrates and all references to SPL in
this document refer to the root mean square unless otherwise noted. SPL
does not take the duration of a sound into account.
Characteristics of the Airgun Pulses
Airguns function by venting high-pressure air into the water which
creates an air bubble. The pressure signature of an individual airgun
consists of a sharp rise and then fall in pressure, followed by several
positive and negative pressure excursions caused by the oscillation of
the resulting air bubble. The oscillation of the air bubble transmits
sounds downward through the seafloor and the amount of sound
transmitted in the near horizontal directions is reduced. However, the
airgun array also emits sounds that travel horizontally toward non-
target areas.
The nominal downward-directed source levels of the airgun arrays
used by NSF and ASC on the Palmer do not represent actual sound levels
that can be measured at any location in the water. Rather, they
represent the level that would be found 1 m (3.3 ft) from a
hypothetical point source emitting the same total amount of sound as is
emitted by the combined GI airguns. The actual received level at any
location in the water near the GI airguns will not exceed the source
level of the strongest individual source. In this case, that will be
about 224.6 dB re 1 [mu]Pam peak, or 229.8 dB re 1 [mu]Pam peak-to-peak
for the two 45 in\3\ airgun array, and 228.2 dB re 1 [mu]Pam peak or
233.5 dB re 1 [mu]Pam peak-to-peak for the two 105 in\3\ airgun array.
However, the difference between rms and peak or peak-to-peak values for
a given pulse depends on the frequency content and duration of the
pulse, among other factors. Actual levels experienced by any organism
more than 1 m from either GI airgun will be significantly lower.
Accordingly, Lamont-Doherty Earth Observatory of Columbia
University (L-DEO) has predicted and modeled the received sound levels
in relation to distance and direction from the two GI airgun array. A
detailed description of L-DEO's modeling for this survey's marine
seismic source arrays for protected species mitigation is provided in
the NSF/USGS PEIS. These are the nominal source levels applicable to
downward propagation. The NSF/USGS PEIS discusses the characteristics
of the airgun pulses. NMFS refers the reviewers to those documents for
additional information.
Predicted Sound Levels for the Airguns
To determine exclusion zones for the airgun array to be used in the
intermediate and deep water of the Gulf of Mexico (GOM), received sound
levels have been modeled by L-DEO for a number of airgun
configurations, including two 45 in\3\ and two 105 in\3\ G airguns, in
relation to distance and direction from the airguns (see Figure 2 and 3
in Attachment B of the IHA application). The model does not allow for
bottom interactions, and is most directly applicable to deep water.
Because the model results are for G airguns, which have more energy
than GI airguns of the same size, those distances overestimate (by
approximately 10%) the distances for the two 45 in\3\ GI airguns and
two 105 in\3\ GI airguns, respectively. Although the distances are
overestimated, no adjustments for this have been made to the radii
distances in Table 2 (below). Based on the modeling, estimates of the
maximum distances from the GI airguns where sound levels of 190, 180,
and 160 dB re 1 [mu]Pa (rms) are predicted to be received in shallow,
intermediate, and deep water are shown in Table 2 (see Table 1 of
Attachment B of the IHA application).
[[Page 468]]
Empirical data concerning the 190, 180, and 160 dB (rms) distances
were acquired for various airgun arrays based on measurements during
the acoustic verification studies conducted by L-DEO in the northern
GOM in 2003 (Tolstoy et al., 2004) and 2007 to 2008 (Tolstoy et al.,
2009; Diebold et al., 2010). Results of the 18 and 36 airgun array are
not relevant for the two GI airguns to be used in the proposed survey.
The empirical data for the 6, 10, 12, and 20 airgun arrays indicate
that, for deep water, the L-DEO model tends to overestimate the
received sound levels at a given distance (Tolstoy et al., 2004).
Measurements were not made for the two GI airgun array in deep water;
however, NSF and ASC proposes to use the buffer and exclusion zones
predicted by L-DEO's model for the proposed GI airgun operations in
deep water, although they are likely conservative given the empirical
results for the other arrays. Using the L-DEO model, Table 2 (below)
shows the distances at which three rms sound levels are expected to be
received from the two GI airguns. The 180 and 190 dB re 1 [mu]Pam (rms)
distances are the safety criteria for potential Level A harassment as
specified by NMFS (2000) and are applicable to cetaceans and pinnipeds,
respectively. If marine mammals are detected within or about to enter
the appropriate exclusion zone, the airguns will be shut-down
immediately.
Table 2 summarizes the predicted distances at which sound levels
(160, 180, and 190 dB [rms]) are expected to be received from the two
airgun array (45 in\3\ or 105 in\3\) operating in shallow (less than
100 m [328 ft]), intermediate (100 to 1,000 m [328 to 3,280 ft]), and
deep water (greater than 1,000 m [3,280 ft]) depths.
Table 2-- Predicted and modeled (two 45 in\3\ and two 105 in\3\ GI
airgun array) distances to which sound levels >=190, 180 and 160 dB re:
1 [mu]Pa (rms) could be received in shallow, intermediate, and deep
water during the proposed low-energy seismic survey in the Dumont
d'Urville Sea of the Southern Ocean, January to March 2014.
--------------------------------------------------------------------------------------------------------------------------------------------------------
Predicted RMS radii distances (m) for 2 GI airgun array
Source and total volume Tow depth Water depth (m) --------------------------------------------------------------------------------
(m) 160 dB 180 dB 190 dB
--------------------------------------------------------------------------------------------------------------------------------------------------------
Two GI Airguns (45 in\3\)......... 3 Shallow (<100)....... 1,176.................... 296...................... 147.
(3,858.3 ft)............. (971.1 ft)............... (482.3 ft).
Two GI Airguns (45 in\3\)......... 3 Intermediate (100 to 600...................... 100...................... 15.
1,000). (1,968.5 ft)............. (328ft).................. (49.2 ft).
Two GI Airguns (45 in\3\)......... 3 Deep (>1,000)........ 400...................... 100...................... 10.
(1,312.3 ft)............. (328 ft)................. (32.8 ft).
Two GI Airguns (105 in\3\)........ 3 Shallow (<100)....... 1,970.................... 511...................... 294.
(6,463.3 ft)............. (1,676.5 ft)............. (964.6 ft).
Two GI Airguns (105 in\3\)........ 3 Intermediate (100 to 1,005.................... 100...................... 30.
1,000). (3,297.2 ft)............. (98.4 ft).
Two GI Airguns (105 in\3\)........ 3 Deep (>1,000)........ 670...................... 100...................... 20.
(2,198.2 ft)............. (65.6 ft).
--------------------------------------------------------------------------------------------------------------------------------------------------------
NMFS expects that acoustic stimuli resulting from the proposed
operation of the two GI airgun array has the potential to harass marine
mammals. NMFS does not expect that the movement of the Palmer, during
the conduct of the low-energy seismic survey, has the potential to
harass marine mammals because of the relatively slow operation speed of
the vessel (approximately 5 kts; 9.3 km/hr; 5.8 mph) during seismic
acquisition.
Bathymetric Survey
Along with the low-energy airgun operations, other additional
geophysical measurements would be made using swath bathymetry,
backscatter sonar imagery, high-resolution sub-bottom profiling
(``CHIRP''), imaging, and magnetometer instruments. In addition,
several other transducer-based instruments onboard the vessel would be
operated continuously during the cruise for operational and
navigational purposes. Operating characteristics for the instruments to
be used are described below.
Single-Beam Echosounder (Knudsen 3260)--The hull-mounted CHIRP
sonar would be operated continuously during all phases of the cruise.
This instrument is operated at 12 kHz for bottom-tracking purposes or
at 3.5 kHz in the sub-bottom profiling mode. The sonar emits energy in
a 30[deg] beam from the bottom of the ship.
Single-Beam Echosounder (Bathy 2000)--The hull-mounted sonar
characteristics of the Bathy 2000 are similar to the Knudsen 3260. Only
one hull-mounted echosounder can be operated a time, and this source
would be operated instead of the Knudsen 3260 only if needed (i.e.,
only one would be in continuous operation during the cruise).
Multi-Beam Sonar (Simrad EM120)--The hull-mounted multi-beam sonar
would be operated continuously during the cruise. This instrument
operates at a frequency of 12 kHz, has an estimated maximum source
energy level of 242 dB re 1[mu]Pa (rms), and emits a very narrow
(<2[deg]) beam fore to aft and 150[deg] in cross-track. The multi-beam
system emits a series of nine consecutive 15 ms pulses.
Acoustic Doppler Current Profiler (ADCP Teledyne RDI VM-150)--The
hull-mounted ADCP would be operated continuously throughout the cruise.
The ADCP operates at a frequency of 150 kHz with an estimated acoustic
output level at the source of 223.6 dB re 1[mu]Pa (rms). Sound energy
from the ADCP is emitted as a 30[deg] conically-shaped beam.
Acoustic Doppler Current Profiler (ADCP Ocean Surveyor OS-38)--The
characteristics of this backup hull-mounted ADCP unit are similar to
the Teledyne VM-150 and would be continuously operated.
Acoustic Locator (Pinger)--An acoustic locator (i.e., pinger) would
be deployed when using the Smith-McIntyre grab sampler and multi-corer
(Mega-corer) to enable these devices to be located in the event they
become detached from their lines. A pinger typically operates at a
frequency of 12 kHz, generates a 5 ms pulse per second, and has an
acoustical output of 162 dB re 1[mu]Pa (rms). A maximum total of 30
samples would be obtained using these devices and require approximately
one hour per sample; therefore, the pinger would operate for a total of
30 hours.
Passive Instruments--During the seismic survey in the Dumont
d'Urville Sea, a precession magnetometer and Air-Sea gravity meter
would be deployed. In addition, numerous (approximately 24) expendable
bathythermograph (XBTs) probes would
[[Page 469]]
also be released (and none would be recovered) over the course of the
cruise to obtain temperature data necessary to calculate sound velocity
profiles used by the multi-beam sonar.
Core and Dredge Sampling
The primary sampling goals involve the acquisition of marine
sediment cores of various lengths up to 25 m (82 ft). It is anticipated
that up to 65 sediment cores and grab samples and 12 rock dredge
samples would be collected as summarized in Table 3 (Table 3 of the IHA
application). Each core or grab sample would require approximately one
hour per sample. All cores and dredges would be deployed using a steel
cable/winch system.
Approximately 75 m\2\ (807.3 ft\2\) of seafloor would be disturbed
by each of four deployments of the dredge at three different sites
(resulting in a total of 900 m\2\ [9,687.5 ft\2\] of affected seafloor
for the project). The selection of the bottom sampling locations and
sampling method would be based on observations of the seafloor,
subsurface reflectivity, sediment type, and accessibility due to ice
and weather conditions. Bottom sampling in the Mertz Glacier area would
be limited to strategically selected locations including possible re-
sampling at a previous core site.
Table 3--Proposed Coring and Dredging Activities in the Dumont d'Urville
Sea
------------------------------------------------------------------------
Sampling device Number of deployments
------------------------------------------------------------------------
Smith-MycIntyre grab sampler............. 10 to 15.
Multi-corer (Mega-corer)................. 10 to 15.
Kasten corer (regular or jumbo).......... 20 to 25.
Jumbo piston corer....................... 8 to 10.
Box cage dredge.......................... 10 to 12.
------------------------------------------------------------------------
Limited sampling of rock material would be conducted using a dredge
that would be towed along the seafloor for short distances
(approximately 50 m [164 ft]) to collect samples of bedrock and ice
rafted debris. The available dredges, which have openings of 0.5 to 1.5
m (1.6 to 4.9 ft), would be deployed on rocky substrates. The locations
of the proposed dredge sites are limited to the inner shelf (southern)
perimeter of three areas: The Mertz Trough and two regions along the
Sabrina Coast. Final selection of dredge sites will include review to
ensure that the seamounts or corals in the area are avoided (AOA,
2011).
The Commission for the Conservation of Antarctic Marine Living
Resources (CCAMLR) has adopted conservation measures (i.e., 22-06, 22-
07, and 22-09) to protect vulnerable marine ecosystems (VME), which
include seamounts, hydrothermal vents, cold water corals, and sponge
fields. The conservation measure 22-07 includes mitigation and
reporting requirements if VME are encountered. The science team would
follow these requirements (see Attachment C of the IHA application) if
VME's are encountered while sampling the sea bottom.
In addition, a camera and towed video system would be deployed at
up to 25 sites. This device would lightly touch the seafloor to
establish a baseline and rise to an optimum elevation to obtain the
desired images.
Water Sampling and Current Measurements
High-resolution conductivity, depth, and temperature (CTD)
measurements would be collected to characterize the summer regional
water mass stratification and circulation, and the meridional exchange
of waters between the oceanic and shelf regimes. These physical
measurements would involve approximately SeaBird CTD system casts
including the use of a lowered ADCP (LADCP).
The LADCP would consist of two Teledyne RDI Workhorse Monitor ADCPs
mounted on the CTD/rosette frame and one oriented upward and the other
downward. The LADCP and frame would be raised and lowered by cable and
winch. The LADCPs would operate at a frequency of 307.2 kHz, with an
estimated output acoustic pressure along each 4 beams of 216.3 dB re
1[mu]Pa at 1 m. The beams are angled at 20 degrees from the centerline
of the ADCP head, with a beam angle of 4 degrees for the individual
beams. Typical pulse duration is 5.7 ms, with a typical repetition rate
of 1.75 s. The upward and downward-looking ADCPs are operated in
master-salve mode so that only one head pings at a time. The LADCP
would be operated approximately one hour at every CTD/rosette station
(maximum of 100 stations) for a total of 100 hours of operation.
These instruments would be used to profile the full water column
for temperature, salinity (conductivity), dissolved oxygen and currents
at a series of transects in the study area. Discrete water samples
would be collected for salinity and dissolved oxygen to monitor CTD/
rosette performance, and for oxygen isotopes to assess meltwater
content. Water samples would also be collected for development and
interpretation of marine sediment proxies using Niskin bottles.
Observations of the thermal structure along other portions of the
cruise track would be made using an underway CTD system and XBTs while
the seafloor is swath-mapped. The number and spacing of stations would
be adjusted according to ocean features discovered through multi-beam
swath mapping and the sea ice conditions. If portions of the study area
are inaccessible to the NBP, a contingency sampling focused on the
inflows of MDCW would be pursued in adjacent shelf troughs.
It is noted that underway ADCP on the Palmer can, under ideal
conditions, obtain profiles of ocean currents to depths greater than
800 m (2,624.7 ft). On continental shelves where depths may be less
than the range of the ADCP, the underway profiles cannot resolve the
deepest 15% of the water column due to side lobe reflections from the
bottom which contaminate the water column Doppler returns. For a depth
of 800 m, expected in the MCDW, currents in the lower 120 m (393.7 ft)
could not be measured by the ship ADCP; therefore, the lowered ADCP can
provide accurate current profiles to within a few meters of the bottom
and provide complete coverage of the velocity field at each CTD
station.
Instrumentation Moorings
Four instrumented moorings would be deployed during the proposed
cruise to measure current, temperature, and salinity (conductivity)
continuously. Two of the moorings would be deployed for approximately
one month (short-term moorings) and two moorings would be deployed for
approximately one year (long-term moorings). The two short-term
moorings and one long-term mooring would include ADCP paired with CTD
recorders, and additional intermediate T (i.e., temperature) recorders.
The characteristics of the ADCP units deployed on the moorings are
similar to the Teledyne VM-150; the moored ADCPs operate at frequencies
of 75 kHz (one unit) and 300 kHz (two units). The fourth mooring would
be equipped with sediment traps, a CTD recorder and intermediate T
recorders, and be deployed for approximately one year (long-term
mooring). The two long-term moorings would be retrieved approximately
one year later by a U.S. Arctic Program (USAP) vessel or collaborators
from other countries.
Subject to sea ice conditions, these moorings would preferably be
placed in front of Totten Glacier, but otherwise as close as possible
inside adjacent cross-shelf troughs. If access to the inner shelf is
not allowed by sea ice conditions we would attempt mooring deployments
within the outer shelf close to the
[[Page 470]]
troughs mouth, where the Totten Glacier is more directly connected to
inflows from the oceanic domain offshore. The two long-term moorings
would be deployed within 16 km of each other. The short-term moorings
would be within a few kilometers of each other and no farther than 32
km (17.3 nmi) from the long-term moorings. All instruments would be
kept at depths below 250 m (820.2 ft) to minimize damage or loss by
icebergs.
The moorings would temporarily attached to anchors and be recovered
using acoustic release mechanisms. The mooring recovery process would
be similar regardless of mooring type or when they would be retrieved.
Locating the moorings and releasing the moorings from the steel
railroad wheel anchors (which would not be recovered) would be
accomplished by transmitting sound over a period of several seconds.
This is done with an acoustic deck command unit that sends a sequence
of coded pulses to the receiving units, the acoustic releases,
connected to the mooring anchors. The acoustic releases response to
acknowledge the receipt of commands from the deck unit is by
transmitting a short sequence of pulses back. Both of the acoustic
units (onboard deck unit and moored releases) operate at frequencies
between approximately 7 and 15 kHz. The beam pattern is approximately
omnidirectional. The acoustic source level is less than 192 dB re
1[mu]Pa at 1 m.
In addition to the U.S. moorings described above, three new
moorings would be deployed on behalf of Australia's national science
agency the Commonwealth of Scientific and Industrial Research
Organisation (CSIRO) Physical Oceanography group in the Totten Glacier
region by the project team. These moorings would be retrieved
approximately one year later by collaborators from other countries.
Also, during this cruise, three CSIRO moorings that were deployed over
a year ago in the western outlet of the Mertz-Ninnis Trough would be
recovered. The recovery process and acoustic sources described above
for the U.S. moorings would be used for recovery of the CSIRO moorings.
Icebreaking
Icebreaking is considered by NMFS to be a continuous sound and NMFS
estimates that harassment occurs when marine mammals are exposed to
continuous sounds at a received sound level of 120 dB SPL or above.
Potential takes of marine mammals may ensue from icebreaking activity
in which the Palmer is expected to engage in Antarctic waters (i.e.,
along the George V and Oates Coast of East Antarctica, >65[deg] South,
between 140[deg] and 165[deg] East). While breaking ice, the noise from
the ship, including impact with ice, engine noise, and propeller
cavitation, will exceed 120 dB (rms) continuously. If icebreaking does
occur in Antarctic waters, NMFS, NSF and ASC expect it will occur
during transit and non-seismic operations to gain access to coring,
dredging, or other sampling locations and not during seismic airgun
operations. The research activities and associated contingencies are
designed to avoid areas of heavy sea ice condition. The buffer zone
(160 dB [rms]) for the marine mammal Level B harassment threshold
during the proposed activities is greater than the calculated radius
during icebreaking. Therefore, if the Palmer breaks ice during seismic
operations within the Antarctic waters (within the Dumont d'Urville Sea
or other areas of the Southern Ocean), the more conservative and larger
radius (i.e., that for seismic operations) will be used and supercede
the buffer zone for icebreaking.
In 2008, acousticians from Scripps Institution of Oceanography
Marine Physical Laboratory and University of New Hampshire Center for
Coastal and Ocean Mapping conducted measurements of SPLs of the Healy
icebreaking under various conditions (Roth and Schmidt, 2010). The
results indicated that the highest mean SPL (185 dB) was measured at
survey speeds of 4 to 4.5 kts in conditions of 5/10 ice and greater.
Mean SPL under conditions where the ship was breaking heavy ice by
backing and ramming was actually lower (180 dB). In addition, when
backing and ramming, the vessel is essentially stationary, so the
ensonified area is limited for a short period (on the order of minutes
to tens of minutes) to the immediate vicinity of the vessel until the
ship breaks free and once again makes headway.
The 120 dB received sound level radius around the Healy while
icebreaking was estimated by researchers (USGS, 2010). Using a
spherical spreading model, a source level of 185 dB decays to 120 dB in
about 1,750 m (5,741.5 ft). This model is corroborated by Roth and
Schmidt (2010). Therefore, as the ship travels through the ice, a watch
3,500 m (11,482.9 ft) wide would be subject to sound levels greater
than or equal to 120 dB. This results in potential exposure of 3,500
km\2\ (1,020.4 nmi\2\) to sounds greater than or equal to 120 dB from
icebreaking.
Data characterizing the sound levels generated by icebreaking
activities conducted by the Palmer are not available; therefore, data
for noise generating from an icebreaking vessel such as the U.S. Coast
Guard Cutter (USCGC) Healy will be used as a proxy. It is noted that
the Palmer is a smaller vessel and has less icebreaking capability than
the U.S. Coast Guard's other polar icebreakers, being only capable of
breaking ice up to 1 m thick at speeds of 3 kts (5.6 km/hr or 3 nmi).
Therefore, the sound levels that may be generated by the Palmer are
expected to be lower than the conservative levels estimated and
measured for the Healy. Researchers will work to minimize time spent
breaking ice as science operations are more difficult to conduct in icy
conditions since the ice noise degrades the quality of the seismic and
ADCP data and time spent breaking ice takes away from time supporting
scientific research. Logistically, if the vessel were in heavy ice
conditions, researchers would not tow the airgun array and streamer, as
this would likely damage equipment and generate noisy data. It is
possible that the seismic survey can be performed in low ice conditions
if the Palmer could generate an open path behind the vessel.
Because the Palmer is not rated to break multi-year ice routinely,
operations generally avoid transiting through older ice (i.e., 2 years
or older, thicker than 1 m). If sea ice is encountered during the
cruise, it is anticipated the Palmer will proceed primarily through one
year sea ice, and possibly some new, very thin ice, and would follow
leads wherever possible. Satellite imagery from the Totten region
documents that sea ice is at its minimum extent during the month of
February. The most recent image for the region, from November 21, 2013,
shows that the sea ice is currently breaking up, with a significant
coastal lead of open water. Based on a maximum sea ice extent of 250 km
(135 nmi) and estimating that NSF and ASC will transit to the innermost
shelf and back into open water twice, a round trip transit in each of
the potential work regions, NSF and ASC estimate that the Palmer will
actively break ice up to a distance of 1,000 km (540 nmi). Based on a
ship's speed of 5 kts under moderate ice conditions, this distance
represents approximately 108 hrs of icebreaking operations. It is noted
that typical transit through areas primarily open water and containing
brash ice or pancake ice will not be considered icebreaking.
[[Page 471]]
Dates, Duration, and Specified Geographic Region
The proposed project and survey sites are located in selected
regions of the Dumont d'Urville Sea in the Southern Ocean off the coast
of East Antarctica and focus on the Totten Glacier and Moscow
University Ice Shelf, located on the Sabrina Coast, from greater than
approximately 64[deg] South and between approximately 95 to 135[deg]
East (see Figure 2 of the IHA application), and the Mertz Glacier and
Cook Ice Shelf systems located on the George V and Oates Coast, from
greater than approximately 65[deg] South and between approximately 140
to 165[deg] East in International Waters. The proposed study sites are
characterized by heavy ice cover, with a seasonal break-up in the ice
that structures biological patterns. The proposed studies would occur
in both areas, or entirely in one or the other, depending on ice
conditions. Figure 3 of the IHA application illustrates the limited
detailed bathymetry of the two study areas. Ice conditions encountered
during the previous surveys in the region limited the area where
bathymetric data could be collected. Water depths in the survey area
range from approximately 100 to 1,000 m, and possibly exceeding 1,000 m
in some areas. There is limited information on the depths in the study
area and therefore more detailed information on bathymetry is not
available. Figures 2 and 3 of the IHA application illustrate the
limited available detailed bathymetry of the two proposed study areas
due to ice conditions encountered during previous surveys in the
region. The proposed seismic survey would be within an area of
approximately 5,628 km\2\ (1,640.9 nmi\2\). This estimate is based on
the maximum number of kilometers for the seismic survey (2,800 km)
times the predicted rms radii (m) based on modeling and empirical
measurements (assuming 100% use of the two 105 in\3\ GI airguns in 100
to 1,000 m water depths) which was calculated to be 1,005 m (3,297.2
ft).
The icebreaking will occur, as necessary, between approximately 66
to 70[deg] South and between 140 to 165[deg] East. The total distance
in the region of the vessel will travel include the proposed seismic
survey and transit to dredging or sampling locations and will represent
approximately 5,600 km (3,023.8 nmi). Based on a maximum sea ice extent
of 250 km (135 nmi) and estimating that NSF and ASC will transit to the
innermost shelf and back into open water twice, a round trip transit in
each of the potential work regions, NSF and ASC estimate that the
Palmer will actively break ice up to a distance of 1,000 km (540 nmi).
Based on a ship's speed of 5 kts under moderate ice conditions, this
distance represents approximately 108 hrs of icebreaking operations.
The Palmer is expected to depart from Hobart, Tasmania on
approximately January 29, 2014 and arrive at Hobart, Tasmania on
approximately March 16, 2014. Research operations would be over a span
of 45-days, including to and from port. Ice-free or very low
concentrations of sea ice are required in order to collect high quality
seismic data and not impede passage of the vessel between sampling
locations. This requirement restricts the cruise to operating in mid to
late austral summer when the ice concentrations are typically the
lowest. Some minor deviation from this schedule is possible, depending
on logistics and weather (i.e., the cruise may depart earlier or be
extended due to poor weather; there could be additional days of seismic
operations if collected data are deemed to be of substandard quality).
Description of the Marine Mammals in the Area of the Proposed Specified
Activity
The marine mammals that generally occur in the proposed action area
belong to three taxonomic groups: Mysticetes (baleen whales),
odontocetes (toothed whales), and pinnipeds (seals and sea lions). The
marine mammal species that potentially occur within the Southern Ocean
in proximity to the proposed action area in the Dumont d'Urville Sea
include 28 species of cetaceans and 6 species of pinnipeds.
The Dumont d'Urville Sea may be a feeding ground for many of these
marine mammals. Many of the species that may be potentially present in
the study area seasonally migrate to higher latitudes along the east
coast of Antarctica. In general, most species (except for the killer
whale) migrate north in the middle of the austral winter and return to
Antarctica in the early austral summer. Some species, particularly
Antarctic minke (Balaenoptera bonaerensis) and killer whales (Orcinus
orca), are expected to be present in higher concentrations along the
ice edge (SCAR, 2002). The 6 species of pinnipeds that are found in the
Southern Ocean and which may be present in the proposed study area
include the crabeater (Lebodon carcinophagus), leopard (Hydrurga
leptonyx), Wedell (Leptonychotes weddellii), Ross (Ommatophoca rossii),
southern elephant (Mirounga leonina), and Antarctic fur seal
(Arctocephalus gazella). Many of these pinniped species breed on either
the pack ice or sub-Antarctic islands. Since the southern elephant seal
and Antarctic fur seal haul-outs and rookeries are located on sub-
Antarctic islands and prefer beaches, they are more common north of the
seasonally shifting pack ice found in the proposed study area;
therefore, these two species have not been considered further. Marine
mammal species listed as endangered under the U.S. Endangered Species
Act of 1973 (ESA; 16 U.S.C. 1531 et seq.), includes the southern right
(Eubalaena australis), humpback (Megaptera novaeangliae), sei
(Balaenoptera borealis), fin (Balaenoptera physalus), blue
(Balaenoptera musculus), and sperm (Physeter macrocephalus) whale. Of
those endangered species, the humpback, sei, fin, blue, and sperm whale
are likely to be encountered in the proposed survey area.
Various national Antarctic research programs along the coast of
East Antarctica have conducted scientific cruises that included data on
marine mammal sightings. These observations were made primarily between
30[deg] East and 170[deg] East and north to 60[deg] South. The reported
cetacean sightings are summarized in Tables 5 to 7 of the IHA
application. For pinnipeds, observations made during a scientific
cruise over a 13-day period in East Antarctica are summarized in Table
8 of the IHA application. These observations were made below 60[deg]
South and between 110[deg] East to 165[deg] East and include sightings
of individual animals in the water as well as individuals that were
hauled-out (i.e., resting on the surface of the sea ice).
Records from the International Whaling Commission's Southern Ocean
Whale and Ecosystem Research (IWC-SOWER) circumpolar cruises were also
considered. In addition to the 14 species known to occur in the Dumont
d'Urville Sea of the Southern Ocean, there are 18 cetacean species with
ranges that are known to occur in the sub-Antarctic waters of the study
area which may also feed and/or migrate to the Southern Ocean during
the austral summer, these include the southern right, pygmy right
(Caperea marginata), Bryde's (Balaenoptera brydei), dwarf minke
(Balaenoptera acutorostrata spp.), pygmy blue (Balaenoptera musculus
brevicauda), pygmy dwarf sperm whale (Kogia breviceps), Arnoux's beaked
(Berardius arnuxii), Blainville's beaked whale (Mesoplodon
densirostris), Cuvier's beaked (Ziphius cavirostris), Shepherd's beaked
(Tasmacetus shepherdi), Southern bottlenose (Hyperoodon planifrons),
Andrew's
[[Page 472]]
beaked (Mesoplodon bowdoini), Hector's beaked (Mesoplodon hectori),
Gray's beaked (Mesoplodon grayi), strap-toothed beaked (Mesoplodon
layardii), spade-toothed beaked (Mesoplodon traversii), southern right
whale dolphin (Lissodelphis peronii), Dusky (Lagenorhynchus obscurus),
and bottlenose dolphin (Tursiops truncatus). However, these species
have not been sighted and are not expected to occur where the proposed
activities would take place. These species are not considered further
in this document. Table 4 (below) presents information on the
abundance, distribution, population status, conservation status, and
population trend of the species of marine mammals that may occur in the
proposed study area during February to March 2014.
Table 4--The Habitat, Regional Abundance, and Conservation Status of Marine Mammals That May Occur In or Near
the Proposed Low-Energy Seismic Survey Area in the Antarctic Area of the Southern Ocean
[See text and Tables 4 in NSF and ASC's application for further details]
----------------------------------------------------------------------------------------------------------------
Population
Species Habitat estimate ESA \1\ MMPA \2\ Population trend
----------------------------------------------------------------------------------------------------------------
Mysticetes:
Southern right whale Coastal, pelagic. 8,000 \3\ to EN......... D.......... Increasing.
(Eubalaena australis). 15,000 \4\.
Pygmy right whale (Caperea Coastal, pelagic. NA............... NL......... NC......... NA.
marginata).
Humpback whale (Megaptera Pelagic, 35,000 to 40,000 EN......... D.......... Increasing.
novaeangliae). nearshore \3\--Worldwide.
waters, and 9,484 \5\--Scotia
banks. Sea and
Antarctica
Peninsula.
Dwarf minke whale Pelagic and NA............... NL......... NC......... NA.
(Balaenoptera coastal.
acutorostrata sub-
species).
Antarctic minke whale Pelagic, ice Several 100,000 NL......... NC......... Stable.
(Balaenoptera floes. \3\--Worldwide.
bonaerensis). 18,125 \5\--
Scotia Sea and
Antarctica
Peninsula.
Bryde's whale Pelagic and NA............... NL......... NC......... NA.
(Balaenoptera brydei). coastal.
Sei whale (Balaenoptera Primarily 80,000 \3\-- EN......... D.......... NA.
borealis). offshore, Worldwide.
pelagic.
Fin whale (Balaenoptera Continental 140,000 \3\-- EN......... D.......... NA.
physalus). slope, pelagic. Worldwide.
4,672 \5\--Scotia
Sea and
Antarctica
Peninsula.
Blue whale (Balaenoptera Pelagic, shelf, 8,000 to 9,000 EN......... D.......... NA.
musculus). coastal. \3\--Worldwide.
1,700 \6\--
Southern Ocean.
Odontocetes:
Sperm whale (Physeter Pelagic, deep sea 360,000 \3\-- EN......... D.......... NA.
macrocephalus). Worldwide.
9,500 \3\--
Antarctic.
Pygmy sperm whale (Kogia Pelagic, slope... NA............... NL......... NC......... NA.
breviceps).
Arnoux's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Berardius arnuxii).
Blainville's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon densirostris).
Cuvier's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Ziphius cavirostris).
Shepherd's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Tasmacetus shepherdi).
Southern bottlenose whale Pelagic.......... 500,000 \3\-- NL......... NC......... NA.
(Hyperoodon planifrons). South of
Antarctic
Convergence.
Andrew's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon bowdoini).
Hector's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon hectori).
Gray's beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon grayi).
Strap-toothed beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon layardii).
Spade-toothed beaked whale Pelagic.......... NA............... NL......... NC......... NA.
(Mesoplodon traversii).
[[Page 473]]
Killer whale (Orcinus Pelagic, shelf, 80,000 \3\--South NL......... NC......... NA.
orca). coastal, pack of Antarctic
ice. Convergence.
25,000 \7\--
Southern Ocean.
Long-finned pilot whale Pelagic, shelf, 200,000 3 8-- NL......... NC......... NA.
(Globicephala melas). coastal. South of
Antarctic
Convergence.
Bottlenose dolphin Offshore, >625,500 \3\-- NL......... NC......... NA.
(Tursiops truncatus). inshore, Worldwide.
coastal,
estuaries.
Southern right whale Pelagic.......... NA............... NL......... NC......... NA.
dolphin (Lissodelphis
peronii).
Dusky dolphin Coastal, NA............... NL......... NC......... NA.
(Lagenorhynchus obscurus). continental
shelf and slope.
Hourglass dolphin Pelatic, ice edge 144,000 \3\...... NL......... NC......... NA.
(Lagenorhynchus cruciger).
Spectacled porpoise Coastal, pelagic. NA............... NL......... NC......... NA.
(Phocoena dioptrica).
Pinnipeds:
Crabeater seal (Lobodon Coastal, pack ice 5,000,000 to NL......... NC......... Increasing.
carcinophaga). 15,000,000 3 9.
Leopard seal (Hydrurga Pack ice, sub- 220,000 to NL......... NC......... NA.
leptonyx). Antarctic 440,000 3 10.
islands.
Ross seal (Ommatophoca Pack ice, smooth 130,000 \3\...... NL......... NC......... NA.
rossii). ice floes,
pelagic.
Wedell seal (Leptonychotes Fast ice, pack 500,000 to NL......... NC......... NA.
weddellii). ice, sub- 1,000,000 3 11.
Antarctic
islands.
Southern elephant seal Coastal, pelagic, 640,000 \12\ to NL......... NC......... Decreasing,
(Mirounga leonina). sub-Antarctic 650,000 \3\. increasing or
waters. stable
depending on
breeding
population.
Antarctic fur seal Shelf, rocky 1,600,000 \13\ to NL......... NC......... Increasing.
(Arctocephalus gazella). habitats. 3,000,000 \3\.
----------------------------------------------------------------------------------------------------------------
NA = Not available or not assessed.
\1\ U.S. Endangered Species Act: EN = Endangered, T = Threatened, DL = Delisted, NL = Not listed.
\2\ U.S. Marine Mammal Protection Act: D = Depleted, S = Strategic, NC = Not Classified.
\3\ Jefferson et al., 2008.
\4\ Kenney, 2009.
\5\ Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR) survey area (Reilly et al.,
2004).
\6\ Sears and Perrin, 2009.
\7\ Ford, 2009.
\8\ Olson, 2009.
\9\ Bengston, 2009.
\10\ Rogers, 2009.
\11\ Thomas and Terhune, 2009.
\12\ Hindell and Perrin, 2009.
\13\ Arnould, 2009.
Refer to sections 3 and 4 of NSF and ASC's IHA application for
detailed information regarding the abundance and distribution,
population status, and life history and behavior of these other marine
mammal species and their occurrence in the proposed project area. The
IHA application also presents how NSF and ASC calculated the estimated
densities for the marine mammals in the proposed survey area. NMFS has
reviewed these data and determined them to be the best available
scientific information for the purposes of the proposed IHA.
Potential Effects on Marine Mammals
Acoustic stimuli generated by the operation of the airguns, which
introduce sound into the marine environment, may have the potential to
cause Level B harassment of marine mammals in the proposed survey area.
The effects of sounds from airgun operations might include one or more
of the following: Tolerance, masking of natural sounds, behavioral
disturbance, temporary or permanent hearing impairment, or non-auditory
physical or physiological effects (Richardson et al., 1995; Gordon et
al., 2004; Nowacek et al., 2007; Southall et al., 2007). Permanent
hearing impairment, in the unlikely event that it occurred, would
constitute injury, but temporary threshold shift (TTS) is not an injury
(Southall et al., 2007). Although the possibility cannot be entirely
excluded, it is unlikely that the proposed project would result in any
cases of temporary or permanent hearing impairment, or any significant
non-auditory physical or physiological effects. Based on the available
data and studies described here, some behavioral disturbance is
expected. A more comprehensive review of these issues can be found in
the ``Programmatic Environmental
[[Page 474]]
Impact Statement/Overseas Environmental Impact Statement prepared for
Marine Seismic Research that is funded by the National Science
Foundation and conducted by the U.S. Geological Survey'' (NSF/USGS,
2011).
Tolerance
Richardson et al. (1995) defines tolerance as the occurrence of
marine mammals in areas where they are exposed to human activities or
man-made noise. In many cases, tolerance develops by the animal
habituating to the stimulus (i.e., the gradual waning of responses to a
repeated or ongoing stimulus) (Richardson, et al., 1995; Thorpe, 1963),
but because of ecological or physiological requirements, many marine
animals may need to remain in areas where they are exposed to chronic
stimuli (Richardson, et al., 1995).
Numerous studies have shown that pulsed sounds from airguns are
often readily detectable in the water at distances of many kilometers.
Several studies have shown that marine mammals at distances more than a
few kilometers from operating seismic vessels often show no apparent
response. That is often true even in cases when the pulsed sounds must
be readily audible to the animals based on measured received levels and
the hearing sensitivity of the marine mammal group. Although various
baleen whales and toothed whales, and (less frequently) pinnipeds have
been shown to react behaviorally to airgun pulses under some
conditions, at other times marine mammals of all three types have shown
no overt reactions. The relative responsiveness of baleen and toothed
whales are quite variable.
Masking
The term masking refers to the inability of a subject to recognize
the occurrence of an acoustic stimulus as a result of the interference
of another acoustic stimulus (Clark et al., 2009). Introduced
underwater sound may, through masking, reduce the effective
communication distance of a marine mammal species if the frequency of
the source is close to that used as a signal by the marine mammal, and
if the anthropogenic sound is present for a significant fraction of the
time (Richardson et al., 1995).
The airguns for the proposed low-energy seismic survey have
dominant frequency components of 2 to 188 Hz. This frequency range
fully overlaps the lower part of the frequency range of odontocete
calls and/or functional hearing (full range about 150 Hz to 180 kHz).
Airguns also produce a small portion of their sound at mid and high
frequencies that overlap most, if not all, frequencies produced by
odontocetes. While it is assumed that mysticetes can detect acoustic
impulses from airguns and vessel sounds (Richardson et al., 1995a),
sub-bottom profilers, pingers, and most of the multi-beam echosounders
would likely be detectable by some mysticetes based on presumed
mysticete hearing sensitivity. Odontocetes are presumably more
sensitive to mid to high frequencies produced by the mulit-beam
echosounders, sub-bottom profilers, and pingers than to the dominant
low frequencies produced by the airguns and vessel. A more
comprehensive review of the relevant background information for
odontocetes appears in Section 3.6.4.3, Section 3.7.4.3 and Appendix E
of the NSF/USGS PEIS (2011).
Masking effects of pulsed sounds (even from large arrays of
airguns) on marine mammal calls and other natural sounds are expected
to be limited. Because of the intermittent nature and low duty cycle of
seismic airgun pulses, animals can emit and receive sounds in the
relatively quiet intervals between pulses. However, in some situations,
reverberation occurs for much or the entire interval between pulses
(e.g., Simard et al., 2005; Clark and Gagnon, 2006) which could mask
calls. Some baleen and toothed whales are known to continue calling in
the presence of seismic pulses, and their calls can usually be heard
between the seismic pulses (e.g., Richardson et al., 1986; McDonald et
al., 1995; Greene et al., 1999; Nieukirk et al., 2004; Smultea et al.,
2004; Holst et al., 2005a,b, 2006; and Dunn and Hernandez, 2009).
However, Clark and Gagnon (2006) reported that fin whales in the North
Atlantic Ocean went silent for an extended period starting soon after
the onset of a seismic survey in the area. Similarly, there has been
one report that sperm whales ceased calling when exposed to pulses from
a very distant seismic ship (Bowles et al., 1994). However, more recent
studies found that they continued calling in the presence of seismic
pulses (Madsen et al., 2002; Tyack et al., 2003; Smultea et al., 2004;
Holst et al., 2006; and Jochens et al., 2008). Dilorio and Clark (2009)
found evidence of increased calling by blue whales during operations by
a lower-energy seismic source (i.e., sparker). Dolphins and porpoises
commonly are heard calling while airguns are operating (e.g., Gordon et
al., 2004; Smultea et al., 2004; Holst et al., 2005a, b; and Potter et
al., 2007). The sounds important to small odontocetes are predominantly
at much higher frequencies than are the dominant components of airgun
sounds, thus limiting the potential for masking.
Pinnipeds have the most sensitive hearing and/or produce most of
their sounds in frequencies higher than the dominant components of
airgun sound, but there is some overlap in the frequencies of the
airgun pulses and the calls. However, the intermittent nature of airgun
pules presumably reduces the potential for masking.
Marine mammals are thought to be able to compensate for masking by
adjusting their acoustic behavior through shifting call frequencies,
increasing call volume, and increasing vocalization rates. For example
blue whales are found to increase call rates when exposed to noise from
seismic surveys in the St. Lawrence Estuary (Dilorio and Clark, 2009).
The North Atlantic right whales (Eubalaena glacialis) exposed to high
shipping noise increased call frequency (Parks et al., 2007), while
some humpback whales respond to low-frequency active sonar playbacks by
increasing song length (Miller et al., 2000). In general, NMFS expects
the masking effects of seismic pulses to be minor, given the normally
intermittent nature of seismic pulses.
Behavioral Disturbance
Marine mammals may behaviorally react to sound when exposed to
anthropogenic noise. Disturbance includes a variety of effects,
including subtle to conspicuous changes in behavior, movement, and
displacement. Reactions to sound, if any, depend on species, state of
maturity, experience, current activity, reproductive state, time of
day, and many other factors (Richardson et al., 1995; Wartzok et al.,
2004; Southall et al., 2007; Weilgart, 2007). These behavioral
reactions are often shown as: Changing durations of surfacing and
dives, number of blows per surfacing, or moving direction and/or speed;
reduced/increased vocal activities; changing/cessation of certain
behavioral activities (such as socializing or feeding); visible startle
response or aggressive behavior (such as tail/fluke slapping or jaw
clapping); avoidance of areas where noise sources are located; and/or
flight responses (e.g., pinnipeds flushing into the water from haul-
outs or rookeries). If a marine mammal does react briefly to an
underwater sound by changing its behavior or moving a small distance,
the impacts of the change are unlikely to be significant to the
individual, let alone the stock or population. However, if a sound
source displaces marine mammals from an important feeding or breeding
area for a
[[Page 475]]
prolonged period, impacts on individuals and populations could be
significant (e.g., Lusseau and Bejder, 2007; Weilgart, 2007).
The biological significance of many of these behavioral
disturbances is difficult to predict, especially if the detected
disturbances appear minor. However, the consequences of behavioral
modification could be expected to be biologically significant if the
change affects growth, survival, and/or reproduction. Some of these
significant behavioral modifications include:
Change in diving/surfacing patterns (such as those thought
to be causing beaked whale stranding due to exposure to military mid-
frequency tactical sonar);
Habitat abandonment due to loss of desirable acoustic
environment; and
Cessation of feeding or social interaction.
The onset of behavioral disturbance from anthropogenic noise
depends on both external factors (characteristics of noise sources and
their paths) and the receiving animals (hearing, motivation,
experience, demography) and is also difficult to predict (Richardson et
al., 1995; Southall et al., 2007). Given the many uncertainties in
predicting the quantity and types of impacts of noise on marine
mammals, it is common practice to estimate how many mammals would be
present within a particular distance of industrial activities and/or
exposed to a particular level of sound. In most cases, this approach
likely overestimates the numbers of marine mammals that would be
affected in some biologically-important manner.
Baleen Whales--Baleen whales generally tend to avoid operating
airguns, but avoidance radii are quite variable (reviewed in Richardson
et al., 1995; Gordon et al., 2004). Whales are often reported to show
no overt reactions to pulses from large arrays of airguns at distances
beyond a few kilometers, even though the airgun pulses remain well
above ambient noise levels out to much longer distances. However,
baleen whales exposed to strong noise pulses from airguns often react
by deviating from their normal migration route and/or interrupting
their feeding and moving away. In the cases of migrating gray
(Eschrichtius robustus) and bowhead (Balaena mysticetus) whales, the
observed changes in behavior appeared to be of little or no biological
consequence to the animals (Richardson, et al., 1995). They simply
avoided the sound source by displacing their migration route to varying
degrees, but within the natural boundaries of the migration corridors.
Studies of gray, bowhead, and humpback whales have shown that
seismic pulses with received levels of 160 to 170 dB re 1 [mu]Pa (rms)
seem to cause obvious avoidance behavior in a substantial fraction of
the animals exposed (Malme et al., 1986, 1988; Richardson et al.,
1995). In many areas, seismic pulses from large arrays of airguns
diminish to those levels at distances ranging from 4 to 15 km (2.2 to
8.1 nmi) from the source. A substantial proportion of the baleen whales
within those distances may show avoidance or other strong behavioral
reactions to the airgun array. Subtle behavioral changes sometimes
become evident at somewhat lower received levels, and studies have
shown that some species of baleen whales, notably bowhead, gray, and
humpback whales, at times, show strong avoidance at received levels
lower than 160 to 170 dB re 1 [mu]Pa (rms).
Researchers have studied the responses of humpback whales to
seismic surveys during migration, feeding during the summer months,
breeding while offshore from Angola, and wintering offshore from
Brazil. McCauley et al. (1998, 2000a) studied the responses of humpback
whales off western Australia to a full-scale seismic survey with a 16
airgun array (2,678 in\3\) and to a single airgun (20 in\3\) with
source level of 227 dB re 1 [micro]Pa (p-p). In the 1998 study, they
documented that avoidance reactions began at 5 to 8 km (2.7 to 4.3 nmi)
from the array, and that those reactions kept most pods approximately 3
to 4 km (1.6 to 2.2 nmi) from the operating seismic boat. In the 2000
study, they noted localized displacement during migration of 4 to 5 km
(2.2 to 2.7 nmi) by traveling pods and 7 to 12 km (3.8 to 6.5 nmi) by
more sensitive resting pods of cow-calf pairs. Avoidance distances with
respect to the single airgun were smaller but consistent with the
results from the full array in terms of the received sound levels. The
mean received level for initial avoidance of an approaching airgun was
140 dB re 1 [mu]Pa (rms) for humpback pods containing females, and at
the mean closest point of approach distance the received level was 143
dB re 1 [mu]Pa (rms). The initial avoidance response generally occurred
at distances of 5 to 8 km (2.7 to 4.3 nmi) from the airgun array and 2
km (1.1 nmi) from the single airgun. However, some individual humpback
whales, especially males, approached within distances of 100 to 400 m
(328 to 1,312 ft), where the maximum received level was 179 dB re 1
[mu]Pa (rms).
Data collected by observers during several seismic surveys in the
Northwest Atlantic showed that sighting rates of humpback whales were
significantly greater during non-seismic periods compared with periods
when a full array was operating (Moulton and Holst, 2010). In addition,
humpback whales were more likely to swim away and less likely to swim
towards a vessel during seismic vs. non-seismic periods (Moulton and
Holst, 2010).
Humpback whales on their summer feeding grounds in southeast Alaska
did not exhibit persistent avoidance when exposed to seismic pulses
from a 1.64-L (100 in\3\) airgun (Malme et al., 1985). Some humpbacks
seemed ``startled'' at received levels of 150 to 169 dB re 1 [mu]Pa.
Malme et al. (1985) concluded that there was no clear evidence of
avoidance, despite the possibility of subtle effects, at received
levels up to 172 dB re 1 [mu]Pa (rms). However, Moulton and Holst
(2010) reported that humpback whales monitored during seismic surveys
in the Northwest Atlantic had lower sighting rates and were most often
seen swimming away from the vessel during seismic periods compared with
periods when airguns were silent.
Studies have suggested that South Atlantic humpback whales
wintering off Brazil may be displaced or even strand upon exposure to
seismic surveys (Engel et al., 2004). The evidence for this was
circumstantial and subject to alternative explanations (IAGC, 2004).
Also, the evidence was not consistent with subsequent results from the
same area of Brazil (Parente et al., 2006), or with direct studies of
humpbacks exposed to seismic surveys in other areas and seasons. After
allowance for data from subsequent years, there was ``no observable
direct correlation'' between strandings and seismic surveys (IWC, 2007:
236).
Reactions of migrating and feeding (but not wintering) gray whales
to seismic surveys have been studied. Malme et al. (1986, 1988) studied
the responses of feeding eastern Pacific gray whales to pulses from a
single 100 in\3\ airgun off St. Lawrence Island in the northern Bering
Sea. They estimated, based on small sample sizes, that 50 percent of
feeding gray whales stopped feeding at an average received pressure
level of 173 dB re 1 [mu]Pa on an (approximate) rms basis, and that 10
percent of feeding whales interrupted feeding at received levels of 163
dB re 1 [micro]Pa (rms). Those findings were generally consistent with
the results of experiments conducted on larger numbers of gray whales
that were migrating along the California coast (Malme et al., 1984;
Malme and Miles, 1985), and western Pacific gray whales
[[Page 476]]
feeding off Sakhalin Island, Russia (Wursig et al., 1999; Gailey et
al., 2007; Johnson et al., 2007; Yazvenko et al., 2007a, b), along with
data on gray whales off British Columbia (Bain and Williams, 2006).
Various species of Balaenoptera (blue, sei, fin, and minke whales)
have occasionally been seen in areas ensonified by airgun pulses
(Stone, 2003; MacLean and Haley, 2004; Stone and Tasker, 2006), and
calls from blue and fin whales have been localized in areas with airgun
operations (e.g., McDonald et al., 1995; Dunn and Hernandez, 2009;
Castellote et al., 2010). Sightings by observers on seismic vessels off
the United Kingdom from 1997 to 2000 suggest that, during times of good
sightability, sighting rates for mysticetes (mainly fin and sei whales)
were similar when large arrays of airguns were shooting versus silent
(Stone, 2003; Stone and Tasker, 2006). However, these whales tended to
exhibit localized avoidance, remaining significantly further (on
average) from the airgun array during seismic operations compared with
non-seismic periods (Stone and Tasker, 2006). Castellote et al. (2010)
reported that singing fin whales in the Mediterranean moved away from
an operating airgun array.
Ship-based monitoring studies of baleen whales (including blue,
fin, sei, minke, and humpback whales) in the Northwest Atlantic found
that overall, this group had lower sighting rates during seismic vs.
non-seismic periods (Moulton and Holst, 2010). Baleen whales as a group
were also seen significantly farther from the vessel during seismic
compared with non-seismic periods, and they were more often seen to be
swimming away from the operating seismic vessel (Moulton and Holst,
2010). Blue and minke whales were initially sighted significantly
farther from the vessel during seismic operations compared to non-
seismic periods; the same trend was observed for fin whales (Moulton
and Holst, 2010). Minke whales were most often observed to be swimming
away from the vessel when seismic operations were underway (Moulton and
Holst, 2010).
Data on short-term reactions by cetaceans to impulsive noises are
not necessarily indicative of long-term or biologically significant
effects. It is not known whether impulsive sounds affect reproductive
rate or distribution and habitat use in subsequent days or years.
However, gray whales have continued to migrate annually along the west
coast of North America with substantial increases in the population
over recent years, despite intermittent seismic exploration (and much
ship traffic) in that area for decades (Appendix A in Malme et al.,
1984; Richardson et al., 1995; Allen and Angliss, 2010). The western
Pacific gray whale population did not seem affected by a seismic survey
in its feeding ground during a previous year (Johnson et al., 2007).
Similarly, bowhead whales have continued to travel to the eastern
Beaufort Sea each summer, and their numbers have increased notably,
despite seismic exploration in their summer and autumn range for many
years (Richardson et al., 1987; Allen and Angliss, 2010). The history
of coexistence between seismic surveys and baleen whales suggests that
brief exposures to sound pulses from any single seismic survey are
unlikely to result in prolonged effects.
Toothed Whales--Little systematic information is available about
reactions of toothed whales to noise pulses. Few studies similar to the
more extensive baleen whale/seismic pulse work summarized above have
been reported for toothed whales. However, there are recent systematic
studies on sperm whales (e.g., Gordon et al., 2006; Madsen et al.,
2006; Winsor and Mate, 2006; Jochens et al., 2008; Miller et al.,
2009). There is an increasing amount of information about responses of
various odontocetes to seismic surveys based on monitoring studies
(e.g., Stone, 2003; Smultea et al., 2004; Moulton and Miller, 2005;
Bain and Williams, 2006; Holst et al., 2006; Stone and Tasker, 2006;
Potter et al., 2007; Hauser et al., 2008; Holst and Smultea, 2008;
Weir, 2008; Barkaszi et al., 2009; Richardson et al., 2009; Moulton and
Holst, 2010).
Seismic operators and PSOs on seismic vessels regularly see
dolphins and other small toothed whales near operating airgun arrays,
but in general there is a tendency for most delphinids to show some
avoidance of operating seismic vessels (e.g., Goold, 1996a,b,c;
Calambokidis and Osmek, 1998; Stone, 2003; Moulton and Miller, 2005;
Holst et al., 2006; Stone and Tasker, 2006; Weir, 2008; Richardson et
al., 2009; Barkaszi et al., 2009; Moulton and Holst, 2010). Some
dolphins seem to be attracted to the seismic vessel and floats, and
some ride the bow wave of the seismic vessel even when large arrays of
airguns are firing (e.g., Moulton and Miller, 2005). Nonetheless, small
toothed whales more often tend to head away, or to maintain a somewhat
greater distance from the vessel, when a large array of airguns is
operating than when it is silent (e.g., Stone and Tasker, 2006; Weir,
2008; Barry et al., 2010; Moulton and Holst, 2010). In most cases, the
avoidance radii for delphinids appear to be small, on the order of one
km or less, and some individuals show no apparent avoidance. Captive
bottlenose dolphins and beluga whales (Delphinapterus leucas) exhibited
changes in behavior when exposed to strong pulsed sounds similar in
duration to those typically used in seismic surveys (Finneran et al.,
2000, 2002, 2005). However, the animals tolerated high received levels
of sound before exhibiting aversive behaviors.
Results of porpoises depend on species. The limited available data
suggest that harbor porpoises (Phocoena phocoena) show stronger
avoidance of seismic operations than do Dall's porpoises (Phocoenoides
dalli) (Stone, 2003; MacLean and Koski, 2005; Bain and Williams, 2006;
Stone and Tasker, 2006). Dall's porpoises seem relatively tolerant of
airgun operations (MacLean and Koski, 2005; Bain and Williams, 2006),
although they too have been observed to avoid large arrays of operating
airguns (Calambokidis and Osmek, 1998; Bain and Williams, 2006). This
apparent difference in responsiveness of these two porpoise species is
consistent with their relative responsiveness to boat traffic and some
other acoustic sources (Richardson et al., 1995; Southall et al.,
2007).
Most studies of sperm whales exposed to airgun sounds indicate that
the sperm whale shows considerable tolerance of airgun pulses (e.g.,
Stone, 2003; Moulton et al., 2005, 2006a; Stone and Tasker, 2006; Weir,
2008). In most cases the whales do not show strong avoidance, and they
continue to call. However, controlled exposure experiments in the Gulf
of Mexico indicate that foraging behavior was altered upon exposure to
airgun sound (Jochens et al., 2008; Miller et al., 2009; Tyack, 2009).
There are almost no specific data on the behavioral reactions of beaked
whales to seismic surveys. However, some northern bottlenose whales
(Hyperoodon ampullatus) remained in the general area and continued to
produce high-frequency clicks when exposed to sound pulses from distant
seismic surveys (Gosselin and Lawson, 2004; Laurinolli and Cochrane,
2005; Simard et al., 2005). Most beaked whales tend to avoid
approaching vessels of other types (e.g., Wursig et al., 1998). They
may also dive for an extended period when approached by a vessel (e.g.,
Kasuya, 1986), although it is uncertain how much longer such dives may
be as compared to dives by undisturbed beaked whales, which also are
often quite long (Baird et al., 2006; Tyack et al., 2006). Based on a
single observation,
[[Page 477]]
Aguilar-Soto et al. (2006) suggested that foraging efficiency of
Cuvier's beaked whales may be reduced by close approach of vessels. In
any event, it is likely that most beaked whales would also show strong
avoidance of an approaching seismic vessel, although this has not been
documented explicitly. In fact, Moulton and Holst (2010) reported 15
sightings of beaked whales during seismic studies in the Northwest
Atlantic; seven of those sightings were made at times when at least one
airgun was operating. There was little evidence to indicate that beaked
whale behavior was affected by airgun operations; sighting rates and
distances were similar during seismic and non-seismic periods (Moulton
and Holst, 2010).
There are increasing indications that some beaked whales tend to
strand when naval exercises involving mid-frequency sonar operation are
ongoing nearby (e.g., Simmonds and Lopez-Jurado, 1991; Frantzis, 1998;
NOAA and USN, 2001; Jepson et al., 2003; Hildebrand, 2005; Barlow and
Gisiner, 2006; see also the ``Stranding and Mortality'' section in this
notice). These strandings are apparently a disturbance response,
although auditory or other injuries or other physiological effects may
also be involved. Whether beaked whales would ever react similarly to
seismic surveys is unknown. Seismic survey sounds are quite different
from those of the sonar in operation during the above-cited incidents.
Odontocete reactions to large arrays of airguns are variable and,
at least for delphinids, seem to be confined to a smaller radius than
has been observed for the more responsive of some mysticetes. However,
other data suggest that some odontocete species, including harbor
porpoises, may be more responsive than might be expected given their
poor low-frequency hearing. Reactions at longer distances may be
particularly likely when sound propagation conditions are conducive to
transmission of the higher frequency components of airgun sound to the
animals' location (DeRuiter et al., 2006; Goold and Coates, 2006; Tyack
et al., 2006; Potter et al., 2007).
Pinnipeds--Pinnipeds are not likely to show a strong avoidance
reaction to the airgun array. Visual monitoring from seismic vessels
has shown only slight (if any) avoidance of airguns by pinnipeds, and
only slight (if any) changes in behavior. In the Beaufort Sea, some
ringed seals avoided an area of 100 m to (at most) a few hundred meters
around seismic vessels, but many seals remained within 100 to 200 m
(328 to 656 ft) of the trackline as the operating airgun array passed
by (e.g., Harris et al., 2001; Moulton and Lawson, 2002; Miller et al.,
2005.). Ringed seal (Pusa hispida) sightings averaged somewhat farther
away from the seismic vessel when the airguns were operating than when
they were not, but the difference was small (Moulton and Lawson, 2002).
Similarly, in Puget Sound, sighting distances for harbor seals (Phoca
vitulina) and California sea lions (Zalophus californianus) tended to
be larger when airguns were operating (Calambokidis and Osmek, 1998).
Previous telemetry work suggests that avoidance and other behavioral
reactions may be stronger than evident to date from visual studies
(Thompson et al., 1998).
During seismic exploration off Nova Scotia, gray seals (Halichoerus
grypus) exposed to noise from airguns and linear explosive charges did
not react strongly (J. Parsons in Greene et al., 1985). Pinnipeds in
both water and air, sometimes tolerate strong noise pulses from non-
explosive and explosive scaring devices, especially if attracted to the
area for feeding and reproduction (Mate and Harvey, 1987; Reeves et
al., 1996). Thus pinnipeds are expected to be rather tolerant of, or
habituate to, repeated underwater sounds from distant seismic sources,
at least when the animals are strongly attracted to the area.
Hearing Impairment and Other Physical Effects
Exposure to high intensity sound for a sufficient duration may
result in auditory effects such as a noise-induced threshold shift--an
increase in the auditory threshold after exposure to noise (Finneran,
Carder, Schlundt, and Ridgway, 2005). Factors that influence the amount
of threshold shift include the amplitude, duration, frequency content,
temporal pattern, and energy distribution of noise exposure. The
magnitude of hearing threshold shift normally decreases over time
following cessation of the noise exposure. The amount of threshold
shift just after exposure is called the initial threshold shift. If the
threshold shift eventually returns to zero (i.e., the threshold returns
to the pre-exposure value), it is called temporary threshold shift
(TTS) (Southall et al., 2007). Researchers have studied TTS in certain
captive odontocetes and pinnipeds exposed to strong sounds (reviewed in
Southall et al., 2007). However, there has been no specific
documentation of TTS let alone permanent hearing damage, i.e.,
permanent threshold shift (PTS), in free-ranging marine mammals exposed
to sequences of airgun pulses during realistic field conditions.
Temporary Threshold Shift--TTS is the mildest form of hearing
impairment that can occur during exposure to a strong sound (Kryter,
1985). While experiencing TTS, the hearing threshold rises and a sound
must be stronger in order to be heard. At least in terrestrial mammals,
TTS can last from minutes or hours to (in cases of strong TTS) days.
For sound exposures at or somewhat above the TTS threshold, hearing
sensitivity in both terrestrial and marine mammals recovers rapidly
after exposure to the noise ends. Few data on sound levels and
durations necessary to elicit mild TTS have been obtained for marine
mammals, and none of the published data concern TTS elicited by
exposure to multiple pulses of sound. Available data on TTS in marine
mammals are summarized in Southall et al. (2007). Table 2 (above)
presents the estimated distances from the Palmer's airguns at which the
received energy level (per pulse, flat-weighted) would be expected to
be greater than or equal to 180 and 190 dB re 1 [mu]Pa (rms).
To avoid the potential for injury, NMFS (1995, 2000) concluded that
cetaceans and pinnipeds should not be exposed to pulsed underwater
noise at received levels exceeding 180 and 190 dB re 1 [mu]Pa (rms).
NMFS believes that to avoid the potential for Level A harassment,
cetaceans and pinnipeds should not be exposed to pulsed underwater
noise at received levels exceeding 180 and 190 dB re 1 [mu]Pa (rms),
respectively. The established 180 and 190 dB (rms) criteria are not
considered to be the levels above which TTS might occur. Rather, they
are the received levels above which, in the view of a panel of
bioacoustics specialists convened by NMFS before TTS measurements for
marine mammals started to become available, one could not be certain
that there would be no injurious effects, auditory or otherwise, to
marine mammals. NMFS also assumes that cetaceans and pinnipeds exposed
to levels exceeding 160 dB re 1 [mu]Pa (rms) may experience Level B
harassment.
For toothed whales, researchers have derived TTS information for
odontocetes from studies on the bottlenose dolphin and beluga. The
experiments show that exposure to a single impulse at a received level
of 207 kPa (or 30 psi, p-p), which is equivalent to 228 dB re 1 Pa (p-
p), resulted in a 7 and 6 dB TTS in the beluga whale at 0.4 and 30 kHz,
respectively. Thresholds returned to within 2 dB of the pre-exposure
level within 4 minutes of the exposure (Finneran et al., 2002). For the
[[Page 478]]
one harbor porpoise tested, the received level of airgun sound that
elicited onset of TTS was lower (Lucke et al., 2009). If these results
from a single animal are representative, it is inappropriate to assume
that onset of TTS occurs at similar received levels in all odontocetes
(cf. Southall et al., 2007). Some cetaceans apparently can incur TTS at
considerably lower sound exposures than are necessary to elicit TTS in
the beluga or bottlenose dolphin.
For baleen whales, there are no data, direct or indirect, on levels
or properties of sound that are required to induce TTS. The frequencies
to which baleen whales are most sensitive are assumed to be lower than
those to which odontocetes are most sensitive, and natural background
noise levels at those low frequencies tend to be higher. As a result,
auditory thresholds of baleen whales within their frequency band of
best hearing are believed to be higher (less sensitive) than are those
of odontocetes at their best frequencies (Clark and Ellison, 2004).
From this, it is suspected that received levels causing TTS onset may
also be higher in baleen whales than those of odontocetes (Southall et
al., 2007).
In pinnipeds, researchers have not measured TTS thresholds
associated with exposure to brief pulses (single or multiple) of
underwater sound. Initial evidence from more prolonged (non-pulse)
exposures suggested that some pinnipeds (harbor seals in particular)
incur TTS at somewhat lower received levels than do small odontocetes
exposed for similar durations (Kastak et al., 1999, 2005; Ketten et
al., 2001). The TTS threshold for pulsed sounds has been indirectly
extimated as being an SEL of approximately 171 dB re 1
[mu]Pa\2\[middot]s (Southall et al., 2007) which would be equivalent to
a single pulse with a received level of approximately 181 to 186 dB re
1 [mu]Pa (rms), or a series of pulses for which the highest rms values
are a few dB lower. Corresponding values for California sea lions and
northern elephant seals (Mirounga angustirostris) are likely to be
higher (Kastak et al., 2005).
Permanent Threshold Shift--When PTS occurs, there is physical
damage to the sound receptors in the ear. In severe cases, there can be
total or partial deafness, whereas in other cases, the animal has an
impaired ability to hear sounds in specific frequency ranges (Kryter,
1985). There is no specific evidence that exposure to pulses of airgun
sound can cause PTS in any marine mammal, even with large arrays of
airguns. However, given the possibility that mammals close to an airgun
array might incur at least mild TTS, there has been further speculation
about the possibility that some individuals occurring very close to
airguns might incur PTS (e.g., Richardson et al., 1995, p. 372ff;
Gedamke et al., 2008). Single or occasional occurrences of mild TTS are
not indicative of permanent auditory damage, but repeated or (in some
cases) single exposures to a level well above that causing TTS onset
might elicit PTS.
Relationships between TTS and PTS thresholds have not been studied
in marine mammals but are assumed to be similar to those in humans and
other terrestrial mammals (Southall et al., 2007). PTS might occur at a
received sound level at least several dBs above that inducing mild TTS
if the animal were exposed to strong sound pulses with rapid rise
times. Based on data from terrestrial mammals, a precautionary
assumption is that the PTS threshold for impulse sounds (such as airgun
pulses as received close to the source) is at least 6 dB higher than
the TTS threshold on a peak-pressure basis, and probably greater than 6
dB (Southall et al., 2007).
Given the higher level of sound necessary to cause PTS as compared
with TTS, it is considerably less likely that PTS would occur. Baleen
whales generally avoid the immediate area around operating seismic
vessels, as do some other marine mammals.
Stranding and Mortality--When a living or dead marine mammal swims
or floats onto shore and becomes ``beached'' or incapable of returning
to sea, the event is termed a ``stranding'' (Geraci et al., 1999;
Perrin and Geraci, 2002; Geraci and Lounsbury, 2005; NMFS, 2007). The
legal definition for a stranding under the MMPA is that ``(A) a marine
mammal is dead and is (i) on a beach or shore of the United States; or
(ii) in waters under the jurisdiction of the United States (including
any navigable waters); or (B) a marine mammal is alive and is (i) on a
beach or shore of the United States and is unable to return to the
water; (ii) on a beach or shore of the United States and, although able
to return to the water is in need of apparent medical attention; or
(iii) in the waters under the jurisdiction of the United States
(including any navigable waters), but is unable to return to its
natural habitat under its own power or without assistance.''
Marine mammals are known to strand for a variety of reasons, such
as infectious agents, biotoxicosis, starvation, fishery interaction,
ship strike, unusual oceanographic or weather events, sound exposure,
or combinations of these stressors sustained concurrently or in series.
However, the cause or causes of most strandings are unknown (Geraci et
al., 1976; Eaton, 1979; Odell et al., 1980; Best, 1982). Numerous
studies suggest that the physiology, behavior, habitat relationships,
age, or condition of cetaceans may cause them to strand or might pre-
dispose them to strand when exposed to another phenomenon. These
suggestions are consistent with the conclusions of numerous other
studies that have demonstrated that combinations of dissimilar
stressors commonly combine to kill an animal or dramatically reduce its
fitness, even though one exposure without the other does not produce
the same result (Chroussos, 2000; Creel, 2005; DeVries et al., 2003;
Fair and Becker, 2000; Foley et al., 2001; Moberg, 2000; Relyea, 2005a,
2005b; Romero, 2004; Sih et al., 2004).
Strandings Associated With Military Active Sonar--Several sources
have published lists of mass stranding events of cetaceans in an
attempt to identify relationships between those stranding events and
military active sonar (Hildebrand, 2004; IWC, 2005; Taylor et al.,
2004). For example, based on a review of stranding records between 1960
and 1995, the International Whaling Commission (2005) identified ten
mass stranding events and concluded that, out of eight stranding events
reported from the mid-1980s to the summer of 2003, seven had been
coincident with the use of mid-frequency active sonar and most involved
beaked whales.
Over the past 12 years, there have been five stranding events
coincident with military mid-frequency active sonar use in which
exposure to sonar is believed to have been a contributing factor to
strandings: Greece (1996); the Bahamas (2000); Madeira (2000); Canary
Islands (2002); and Spain (2006). Refer to Cox et al. (2006) for a
summary of common features shared by the strandings events in Greece
(1996), Bahamas (2000), Madeira (2000), and Canary Islands (2002); and
Fernandez et al., (2005) for an additional summary of the Canary
Islands 2002 stranding event.
Potential for Stranding From Seismic Surveys--Marine mammals close
to underwater detonations of high explosives can be killed or severely
injured, and the auditory organs are especially susceptible to injury
(Ketten et al., 1993; Ketten, 1995). However, explosives are no longer
used in marine waters for commercial seismic surveys or (with rare
exceptions) for seismic research. These methods have been replaced
entirely by airguns or related non-explosive pulse generators. Airgun
[[Page 479]]
pulses are less energetic and have slower rise times, and there is no
specific evidence that they can cause serious injury, death, or
stranding even in the case of large airgun arrays. However, the
association of strandings of beaked whales with naval exercises
involving mid-frequency active sonar (non-pulse sound) and, in one
case, the co-occurrence of an L-DEO seismic survey (Malakoff, 2002; Cox
et al., 2006), has raised the possibility that beaked whales exposed to
strong ``pulsed'' sounds could also be susceptible to injury and/or
behavioral reactions that can lead to stranding (e.g., Hildebrand,
2005; Southall et al., 2007).
Specific sound-related processes that lead to strandings and
mortality are not well documented, but may include:
(1) Swimming in avoidance of a sound into shallow water;
(2) A change in behavior (such as a change in diving behavior) that
might contribute to tissue damage, gas bubble formation, hypoxia,
cardiac arrhythmia, hypertensive hemorrhage or other forms of trauma;
(3) A physiological change such as a vestibular response leading to
a behavioral change or stress-induced hemorrhagic diathesis, leading in
turn to tissue damage; and
(4) Tissue damage directly from sound exposure, such as through
acoustically-mediated bubble formation and growth or acoustic resonance
of tissues.
Some of these mechanisms are unlikely to apply in the case of
impulse sounds. However, there are indications that gas-bubble disease
(analogous to ``the bends''), induced in supersaturated tissue by a
behavioral response to acoustic exposure, could be a pathologic
mechanism for the strandings and mortality of some deep-diving
cetaceans exposed to sonar. The evidence for this remains
circumstantial and associated with exposure to naval mid-frequency
sonar, not seismic surveys (Cox et al., 2006; Southall et al., 2007).
Seismic pulses and mid-frequency sonar signals are quite different,
and some mechanisms by which sonar sounds have been hypothesized to
affect beaked whales are unlikely to apply to airgun pulses. Sounds
produced by airgun arrays are broadband impulses with most of the
energy below one kHz. Typical military mid-frequency sonar emits non-
impulse sounds at frequencies of 2 to 10 kHz, generally with a
relatively narrow bandwidth at any one time. A further difference
between seismic surveys and naval exercises is that naval exercises can
involve sound sources on more than one vessel. Thus, it is not
appropriate to expect that the same to marine mammals will result from
military sonar and seismic surveys. However, evidence that sonar
signals can, in special circumstances, lead (at least indirectly) to
physical damage and mortality (e.g., Balcomb and Claridge, 2001; NOAA
and USN, 2001; Jepson et al., 2003; Fern[aacute]ndez et al., 2004,
2005; Hildebrand 2005; Cox et al., 2006) suggests that caution is
warranted when dealing with exposure of marine mammals to any high-
intensity sound.
There is no conclusive evidence of cetacean strandings or deaths at
sea as a result of exposure to seismic surveys, but a few cases of
strandings in the general area where a seismic survey was ongoing have
led to speculation concerning a possible link between seismic surveys
and strandings. Suggestions that there was a link between seismic
surveys and strandings of humpback whales in Brazil (Engel et al.,
2004) were not well founded (IAGC, 2004; IWC, 2007). In September 2002,
there was a stranding of two Cuvier's beaked whales in the Gulf of
California, Mexico, when the L-DEO vessel R/V Maurice Ewing was
operating a 20 airgun (8,490 in\3\) array in the general area. The link
between the stranding and the seismic surveys was inconclusive and not
based on any physical evidence (Hogarth, 2002; Yoder, 2002).
Nonetheless, the Gulf of California incident plus the beaked whale
strandings near naval exercises involving use of mid-frequency sonar
suggests a need for caution in conducting seismic surveys in areas
occupied by beaked whales until more is known about effects of seismic
surveys on those species (Hildebrand, 2005). No injuries of beaked
whales are anticipated during the proposed study because of:
(1) The high likelihood that any beaked whales nearby would avoid
the approaching vessel before being exposed to high sound levels, and
(2) Differences between the sound sources operated by L-DEO and
those involved in the naval exercises associated with strandings.
Non-auditory Physiological Effects--Non-auditory physiological
effects or injuries that theoretically might occur in marine mammals
exposed to strong underwater sound include stress, neurological
effects, bubble formation, resonance, and other types of organ or
tissue damage (Cox et al., 2006; Southall et al., 2007). Studies
examining such effects are limited. However, resonance effects (Gentry,
2002) and direct noise-induced bubble formations (Crum et al., 2005)
are implausible in the case of exposure to an impulsive broadband
source like an airgun array. If seismic surveys disrupt diving patterns
of deep-diving species, this might perhaps result in bubble formation
and a form of the bends, as speculated to occur in beaked whales
exposed to sonar. However, there is no specific evidence of this upon
exposure to airgun pulses.
In general, very little is known about the potential for seismic
survey sounds (or other types of strong underwater sounds) to cause
non-auditory physical effects in marine mammals. Such effects, if they
occur at all, would presumably be limited to short distances and to
activities that extend over a prolonged period. The available data do
not allow identification of a specific exposure level above which non-
auditory effects can be expected (Southall et al., 2007), or any
meaningful quantitative predictions of the numbers (if any) of marine
mammals that might be affected in those ways. Marine mammals that show
behavioral avoidance of seismic vessels, including most baleen whales,
some odontocetes, and some pinnipeds, are especially unlikely to incur
non-auditory physical effects.
Potential Effects of Other Acoustic Devices and Sources
Multibeam Echosounder
NSF and ASC will operate the Simrad EM120 multibeam echosounder
from the source vessel during the planned study. Sounds from the
multibeam echosounder are very short pulses, occurring for 15 ms,
depending on water depth. Most of the energy in the sound pulses
emitted by the multibeam echosounder is at frequencies near 12 kHz, and
the maximum source level is 242 dB re 1 [mu]Pa (rms). The beam is
narrow (1 to 2[deg]) in fore-aft extent and wide (150[deg]) in the
cross-track extent. Each ping consists of nine (in water greater than
1,000 m deep) consecutive successive fan-shaped transmissions
(segments) at different cross-track angles. Any given mammal at depth
near the trackline would be in the main beam for only one or two of the
nine segments. Also, marine mammals that encounter the Simrad EM120 are
unlikely to be subjected to repeated pulses because of the narrow fore-
aft width of the beam and will receive only limited amounts of pulse
energy because of the short pulses. Animals close to the ship (where
the beam is narrowest) are especially unlikely to be ensonified for
more than one 15 ms pulse (or two pulses if in the overlap area).
Similarly, Kremser et al. (2005) noted that the probability of a
cetacean swimming through the area of exposure when a multibeam
echosounder emits a
[[Page 480]]
pulse is small. The animal would have to pass the transducer at close
range and be swimming at speeds similar to the vessel in order to
receive the multiple pulses that might result in sufficient exposure to
cause TTS.
Navy sonars that have been linked to avoidance reactions and
stranding of cetaceans: (1) Generally have longer pulse duration than
the Simrad EM120; and (2) are often directed close to horizontally, as
well as omnidirectional, versus more downward and narrowly for the
multibeam echosounder. The area of possible influence of the multibeam
echosounder is much smaller--a narrow band below the source vessel.
Also, the duration of exposure for a given marine mammal can be much
longer for naval sonar. During NSF and ASC's operations, the individual
pulses will be very short, and a given mammal would not receive many of
the downward-directed pulses as the vessel passes by. Possible effects
of a multibeam echosounder on marine mammals are described below.
Masking--Marine mammal communications will not be masked
appreciably by the multibeam echosounder signals given the low duty
cycle of the echosounder and the brief period when an individual mammal
is likely to be within its beam. Furthermore, in the case of baleen
whales, the multibeam echosounder signals (12 kHz) do not overlap with
the predominant frequencies in the calls, which would avoid any
significant masking.
Behavioral Responses--Behavioral reactions of free-ranging marine
mammals to sonars, echosounders, and other sound sources appear to vary
by species and circumstance. Observed reactions have included silencing
and dispersal by sperm whales (Watkins et al., 1985), increased
vocalizations and no dispersal by pilot whales (Rendell and Gordon,
1999), and the previously-mentioned beachings by beaked whales. During
exposure to a 21 to 25 kHz ``whale-finding'' sonar with a source level
of 215 dB re 1 [mu]Pa, gray whales reacted by orienting slightly away
from the source and being deflected from their course by approximately
200 m (656.2 ft) (Frankel, 2005). When a 38 kHz echosounder and a 150
kHz acoustic Doppler current profiler were transmitting during studies
in the Eastern Tropical Pacific, baleen whales showed no significant
responses, while spotted and spinner dolphins were detected slightly
more often and beaked whales less often during visual surveys
(Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a beluga whale exhibited changes in
behavior when exposed to 1 second tonal signals at frequencies similar
to those that will be emitted by the multibeam echosounder used by NSF
and ASC, and to shorter broadband pulsed signals. Behavioral changes
typically involved what appeared to be deliberate attempts to avoid the
sound exposure (Schlundt et al., 2000; Finneran et al., 2002; Finneran
and Schlundt, 2004). The relevance of those data to free-ranging
odontocetes is uncertain, and in any case, the test sounds were quite
different in duration as compared with those from a multibeam
echosounder.
Hearing Impairment and Other Physical Effects--Given several
stranding events that have been associated with the operation of naval
sonar in specific circumstances, there is concern that mid-frequency
sonar sounds can cause serious impacts to marine mammals (see above).
However, the multibeam echosounder proposed for use by NSF and ASC is
quite different than sonar used for Navy operations. Pulse duration of
the multibeam echosounder is very short relative to the naval sonar.
Also, at any given location, an individual marine mammal would be in
the beam of the multibeam echosounder for much less time given the
generally downward orientation of the beam and its narrow fore-aft
beamwidth; Navy sonar often uses near-horizontally-directed sound.
Those factors would all reduce the sound energy received from the
multibeam echosounder rather drastically relative to that from naval
sonar.
NMFS believes that the brief exposure of marine mammals to one
pulse, or small numbers of signals, from the multi-beam echosounder in
this particular case is not likely to result in the harassment of
marine mammals.
Single-Beam Echosounder
NSF and ASC will operate the Knudsen 3260 and Bathy 2000 single-
beam echosounders from the source vessel during the planned study.
Sounds from the single-beam echosounder are very short pulses,
depending on water depth. Most of the energy in the sound pulses
emitted by the singlebeam echosounder is at frequencies near 12 kHz for
bottom-tracking purposes or at 3.5 kHz in the sub-bottom profiling
mode. The sonar emits energy in a 30[deg] beam from the bottom of the
ship. Marine mammals that encounter the Simrad EM120 are unlikely to be
subjected to repeated pulses because of the narrow fore-aft width of
the beam and will receive only limited amounts of pulse energy because
of the short pulses. Animals close to the ship (where the beam is
narrowest) are especially unlikely to be ensonified for more than one
15 ms pulse (or two pulses if in the overlap area). Similarly, Kremser
et al. (2005) noted that the probability of a cetacean swimming through
the area of exposure when a multibeam echosounder emits a pulse is
small. The animal would have to pass the transducer at close range and
be swimming at speeds similar to the vessel in order to receive the
multiple pulses that might result in sufficient exposure to cause TTS.
Navy sonars that have been linked to avoidance reactions and
stranding of cetaceans: (1) Generally have longer pulse duration than
the Simrad EM120; and (2) are often directed close to horizontally
versus more downward for the echosounder. The area of possible
influence of the single-beam echosounder is much smaller--a narrow band
below the source vessel. Also, the duration of exposure for a given
marine mammal can be much longer for naval sonar. During NSF and ASC's
operations, the individual pulses will be very short, and a given
mammal would not receive many of the downward-directed pulses as the
vessel passes by. Possible effects of a single-beam echosounder on
marine mammals are described below.
Masking--Marine mammal communications will not be masked
appreciably by the single-beam echosounder signals given the low duty
cycle of the echosounder and the brief period when an individual mammal
is likely to be within its beam. Furthermore, in the case of baleen
whales, the single-beam echosounder signals (12 or 3.5 kHz) do not
overlap with the predominant frequencies in the calls, which would
avoid any significant masking.
Behavioral Responses--Behavioral reactions of free-ranging marine
mammals to sonars, echosounders, and other sound sources appear to vary
by species and circumstance. Observed reactions have included silencing
and dispersal by sperm whales (Watkins et al., 1985), increased
vocalizations and no dispersal by pilot whales (Rendell and Gordon,
1999), and the previously-mentioned beachings by beaked whales. During
exposure to a 21 to 25 kHz ``whale-finding'' sonar with a source level
of 215 dB re 1 [micro]Pa, gray whales reacted by orienting slightly
away from the source and being deflected from their course by
approximately 200 m (656.2 ft) (Frankel, 2005). When a 38 kHz
echosounder and a 150 kHz ADCP were transmitting during studies in the
Eastern Tropical Pacific, baleen whales
[[Page 481]]
showed no significant responses, while spotted and spinner dolphins
were detected slightly more often and beaked whales less often during
visual surveys (Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a beluga whale exhibited changes in
behavior when exposed to 1 second tonal signals at frequencies similar
to those that will be emitted by the single-beam echosounder used by
NSF and ASC, and to shorter broadband pulsed signals. Behavioral
changes typically involved what appeared to be deliberate attempts to
avoid the sound exposure (Schlundt et al., 2000; Finneran et al., 2002;
Finneran and Schlundt, 2004). The relevance of those data to free-
ranging odontocetes is uncertain, and in any case, the test sounds were
quite different in duration as compared with those from a single-beam
echosounder.
Hearing Impairment and Other Physical Effects--Given recent
stranding events that have been associated with the operation of naval
sonar, there is concern that mid-frequency sonar sounds can cause
serious impacts to marine mammals (see above). However, the single-beam
echosounder proposed for use by NSF and ASC is quite different than
sonar used for Navy operations. Pulse duration of the single-beam
echosounder is very short relative to the naval sonar. Also, at any
given location, an individual marine mammal would be in the beam of the
single-beam echosounder for much less time given the generally downward
orientation of the beam and its narrow fore-aft beamwidth; Navy sonar
often uses near-horizontally-directed sound. Those factors would all
reduce the sound energy received from the single-beam echosounder
rather drastically relative to that from naval sonar.
NMFS believes that the brief exposure of marine mammals to one
pulse, or small numbers of signals, from the single-beam echosounder in
this particular case is not likely to result in the harassment of
marine mammals.
Acoustic Doppler Current Profilers
NSF and ASC will operate the ADCP Teledyne RDI VM-150 and ADCP
Ocean Surveyor OS-38 from the source vessel during the planned study.
Most of the energy in the sound pulses emitted by the ADCPs operate at
frequencies near 150 kHz, and the maximum source level is 223.6 dB re 1
[mu]Pa (rms). Sound energy from the ADCP is emitted as a 30[deg]
conically-shaped beam. Marine mammals that encounter the ADCPs are
unlikely to be subjected to repeated pulses because of the narrow fore-
aft width of the beam and will receive only limited amounts of pulse
energy because of the short pulses. Animals close to the ship (where
the beam is narrowest) are especially unlikely to be ensonified for
more than one 15 ms pulse (or two pulses if in the overlap area).
Similarly, Kremser et al. (2005) noted that the probability of a
cetacean swimming through the area of exposure when the ADCPs emits a
pulse is small. The animal would have to pass the transducer at close
range and be swimming at speeds similar to the vessel in order to
receive the multiple pulses that might result in sufficient exposure to
cause TTS.
Navy sonars that have been linked to avoidance reactions and
stranding of cetaceans: (1) Generally have longer pulse duration than
the ADCPs; and (2) are often directed close to horizontally versus more
downward for the ADCPs. The area of possible influence of the multibeam
echosounder is much smaller--a narrow band below the source vessel.
Also, the duration of exposure for a given marine mammal can be much
longer for naval sonar. During NSF and ASC's operations, the individual
pulses will be very short, and a given mammal would not receive many of
the downward-directed pulses as the vessel passes by. Possible effects
of the ADCPs on marine mammals are described below.
Masking--Marine mammal communications will not be masked
appreciably by the ADCP signals given the low duty cycle of the ADCPs
and the brief period when an individual mammal is likely to be within
its beam. Furthermore, in the case of baleen whales, the ADCP signals
(150 kHz) do not overlap with the predominant frequencies in the calls,
which would avoid any significant masking.
Behavioral Responses--Behavioral reactions of free-ranging marine
mammals to sonars, echosounders, and other sound sources appear to vary
by species and circumstance. Observed reactions have included silencing
and dispersal by sperm whales (Watkins et al., 1985), increased
vocalizations and no dispersal by pilot whales (Rendell and Gordon,
1999), and the previously-mentioned beachings by beaked whales. During
exposure to a 21 to 25 kHz ``whale-finding'' sonar with a source level
of 215 dB re 1 [micro]Pa, gray whales reacted by orienting slightly
away from the source and being deflected from their course by
approximately 200 m (656.2 ft) (Frankel, 2005). When a 38 kHz
echosounder and a 150 kHz ADCP were transmitting during studies in the
Eastern Tropical Pacific, baleen whales showed no significant
responses, while spotted and spinner dolphins were detected slightly
more often and beaked whales less often during visual surveys
(Gerrodette and Pettis, 2005).
Captive bottlenose dolphins and a beluga whale exhibited changes in
behavior when exposed to 1 second tonal signals at frequencies similar
to those that will be emitted by the multibeam echosounder used by NSF
and ASC, and to shorter broadband pulsed signals. Behavioral changes
typically involved what appeared to be deliberate attempts to avoid the
sound exposure (Schlundt et al., 2000; Finneran et al., 2002; Finneran
and Schlundt, 2004). The relevance of those data to free-ranging
odontocetes is uncertain, and in any case, the test sounds were quite
different in duration as compared with those from a multibeam
echosounder.
Hearing Impairment and Other Physical Effects--Given recent
stranding events that have been associated with the operation of naval
sonar, there is concern that mid-frequency sonar sounds can cause
serious impacts to marine mammals (see above). However, the multibeam
echosounder proposed for use by NSF and ASC is quite different than
sonar used for Navy operations. Pulse duration of the ADCP is very
short relative to the naval sonar. Also, at any given location, an
individual marine mammal would be in the beam of the multibeam
echosounder for much less time given the generally downward orientation
of the beam and its narrow fore-aft beamwidth; Navy sonar often uses
near-horizontally-directed sound. Those factors would all reduce the
sound energy received from the multibeam echosounder rather drastically
relative to that from naval sonar.
NMFS believes that the brief exposure of marine mammals to one
pulse, or small numbers of signals, from the multi-beam echosounder in
this particular case is not likely to result in the harassment of
marine mammals.
Acoustic Locator
NSF and ASC will operate the acoustic locator from the source
vessel during the planned study during sampling. Sounds from the
locator are very short pulses, occurring for 5 ms. Most of the energy
in the sound pulses emitted by the acoustic locator is at frequencies
near 12 kHz, and the maximum source level is 162 dB re 1 [mu]Pa (rms).
Animals close to the ship (where the beam is narrowest) are especially
unlikely to be ensonified for more than one 5 ms pulse (or two pulses
if in the overlap area). Similarly, Kremser et al. (2005) noted that
the probability of a cetacean swimming through the area of exposure
when a
[[Page 482]]
multibeam echosounder emits a pulse is small. The animal would have to
pass the transducer at close range and be swimming at speeds similar to
the vessel in order to receive the multiple pulses that might result in
sufficient exposure to cause TTS.
Masking--Marine mammal communications will not be masked
appreciably by the acoustic locator signals given the low duty cycle
and the low source level. Furthermore, in the case of baleen whales,
the acoustic locator signals (12 kHz) do not overlap with the
predominant frequencies in the calls, which would avoid any significant
masking.
Behavioral Responses--Behavioral reactions of free-ranging marine
mammals to sonars, echosounders, and other sound sources appear to vary
by species and circumstance. Observed reactions have included silencing
and dispersal by sperm whales (Watkins et al., 1985), increased
vocalizations and no dispersal by pilot whales (Rendell and Gordon,
1999), and the previously-mentioned beachings by beaked whales. During
exposure to a 21 to 25 kHz ``whale-finding'' sonar with a source level
of 215 dB re 1 [micro]Pa, gray whales reacted by orienting slightly
away from the source and being deflected from their course by
approximately 200 m (656.2 ft) (Frankel, 2005). When a 38 kHz
echosounder and a 150 kHz ADCP were transmitting during studies in the
Eastern Tropical Pacific, baleen whales showed no significant
responses, while spotted and spinner dolphins were detected slightly
more often and beaked whales less often during visual surveys
(Gerrodette and Pettis, 2005).
NMFS believes that the brief exposure of marine mammals to one
pulse, or small numbers of signals, from the acoustic locator is not
likely to result in the harassment of marine mammals.
Core and Dredge Sampling
During coring and dredging, the noise created by the mechanical
action of the devices on the seafloor is expected to be perceived by
nearby fish and other marine organisms and deter them from swimming
toward the source. Coring and dredging activities would be highly
localized and short-term in duration and would not be expected to
significantly interfere with marine mammal behavior. The potential
direct effects include temporary localized disturbance or displacement
from associated sounds and/or physical movement/actions of the
operations. Additionally, the potential indirect effects may consist of
very localized and transitory/short-term disturbance of bottom habitat
and associated prey in shallow-water areas as a result of coring,
dredging, and sediment sampling (NSF/USGS PEIS, 2011). NMFS believes
that the brief exposure of marine mammals to noise created from the
mechanical action of the devices for core and dredge sampling is not
likely to result in the harassment of marine mammals.
Vessel Movement and Collisions
Vessel movement in the vicinity of marine mammals has the potential
to result in either a behavioral response or a direct physical
interaction. Both scenarios are discussed below in this section.
Behavioral Responses to Vessel Movement--There are limited data
concerning marine mammal behavioral responses to vessel traffic and
vessel noise, and a lack of consensus among scientists with respect to
what these responses mean or whether they result in short-term or long-
term adverse effects. In those cases where there is a busy shipping
lane or where there is a large amount of vessel traffic, marine mammals
(especially low frequency specialists) may experience acoustic masking
(Hildebrand, 2005) if they are present in the area (e.g., killer whales
in Puget Sound; Foote et al., 2004; Holt et al., 2008). In cases where
vessels actively approach marine mammals (e.g., whale watching or
dolphin watching boats), scientists have documented that animals
exhibit altered behavior such as increased swimming speed, erratic
movement, and active avoidance behavior (Bursk, 1983; Acevedo, 1991;
Baker and MacGibbon, 1991; Trites and Bain, 2000; Williams et al.,
2002; Constantine et al., 2003), reduced blow interval (Ritcher et al.,
2003), disruption of normal social behaviors (Lusseau, 2003, 2006), and
the shift of behavioral activities which may increase energetic costs
(Constantine et al., 2003, 2004). A detailed review of marine mammal
reactions to ships and boats is available in Richardson et al., (1995).
For each of the marine mammal taxonomy groups, Richardson et al.,
(1995) provides the following assessment regarding reactions to vessel
traffic:
Toothed whales--``In summary, toothed whales sometimes show no
avoidance reaction to vessels, or even approach them. However,
avoidance can occur, especially in response to vessels of types used to
chase or hunt the animals. This may cause temporary displacement, but
we know of no clear evidence that toothed whales have abandoned
significant parts of their range because of vessel traffic.''
Baleen whales--``When baleen whales receive low-level sounds from
distant or stationary vessels, the sounds often seem to be ignored.
Some whales approach the sources of these sounds. When vessels approach
whales slowly and non-aggressively, whales often exhibit slow and
inconspicuous avoidance maneuvers. In response to strong or rapidly
changing vessel noise, baleen whales often interrupt their normal
behavior and swim rapidly away. Avoidance is especially strong when a
boat heads directly toward the whale.''
Behavioral responses to stimuli are complex and influenced to
varying degrees by a number of factors, such as species, behavioral
contexts, geographical regions, source characteristics (moving or
stationary, speed, direction, etc.), prior experience of the animal and
physical status of the animal. For example, studies have shown that
beluga whales' reaction varied when exposed to vessel noise and
traffic. In some cases, beluga whales exhibited rapid swimming from
ice-breaking vessels up to 80 km (43.2 nmi) away and showed changes in
surfacing, breathing, diving, and group composition in the Canadian
high Arctic where vessel traffic is rare (Finley et al., 1990). In
other cases, beluga whales were more tolerant of vessels, but responded
differentially to certain vessels and operating characteristics by
reducing their calling rates (especially older animals) in the St.
Lawrence River where vessel traffic is common (Blane and Jaakson,
1994). In Bristol Bay, Alaska, beluga whales continued to feed when
surrounded by fishing vessels and resisted dispersal even when
purposefully harassed (Fish and Vania, 1971).
In reviewing more than 25 years of whale observation data, Watkins
(1986) concluded that whale reactions to vessel traffic were ``modified
by their previous experience and current activity: habituation often
occurred rapidly, attention to other stimuli or preoccupation with
other activities sometimes overcame their interest or wariness of
stimuli.'' Watkins noticed that over the years of exposure to ships in
the Cape Cod area, minke whales changed from frequent positive interest
(e.g., approaching vessels) to generally uninterested reactions; fin
whales changed from mostly negative (e.g., avoidance) to uninterested
reactions; fin whales changed from mostly negative (e.g., avoidance) to
uninterested reactions; right whales apparently continued the same
variety of responses (negative, uninterested, and positive responses)
with little change; and humpbacks dramatically changed from mixed
responses that were often
[[Page 483]]
negative to reactions that were often strongly positive. Watkins (1986)
summarized that ``whales near shore, even in regions with low vessel
traffic, generally have become less wary of boats and their noises, and
they have appeared to be less easily disturbed than previously. In
particular locations with intense shipping and repeated approaches by
boats (such as the whale-watching areas of Stellwagen Bank), more and
more whales had positive reactions to familiar vessels, and they also
occasionally approached other boats and yachts in the same ways.''
Although the radiated sound from the Palmer will be audible to
marine mammals over a large distance, it is unlikely that marine
mammals will respond behaviorally (in a manner that NMFS would consider
harassment under the MMPA) to low-level distant shipping noise as the
animals in the area are likely to be habituated to such noises (Nowacek
et al., 2004). In light of these facts, NMFS does not expect the
Palmer's movements to result in Level B harassment.
Vessel Strike--Ship strikes of cetaceans can cause major wounds,
which may lead to the death of the animal. An animal at the surface
could be struck directly by a vessel, a surfacing animal could hit the
bottom of a vessel, or an animal just below the surface could be cut by
a vessel's propeller. The severity of injuries typically depends on the
size and speed of the vessel (Knowlton and Kraus, 2001; Laist et al.,
2001; Vanderlaan and Taggart, 2007).
The most vulnerable marine mammals are those that spend extended
periods of time at the surface in order to restore oxygen levels within
their tissues after deep dives (e.g., the sperm whale). In addition,
some baleen whales, such as the North Atlantic right whale, seem
generally unresponsive to vessel sound, making them more susceptible to
vessel collisions (Nowacek et al., 2004). These species are primarily
large, slow moving whales. Smaller marine mammals (e.g., bottlenose
dolphin) move quickly through the water column and are often seen
riding the bow wave of large ships. Marine mammal responses to vessels
may include avoidance and changes in dive pattern (NRC, 2003).
An examination of all known ship strikes from all shipping sources
(civilian and military) indicates vessel speed is a principal factor in
whether a vessel strike results in death (Knowlton and Kraus, 2001;
Laist et al., 2001; Jensen and Silber, 2003; Vanderlaan and Taggart,
2007). In assessing records in which vessel speed was known, Laist et
al. (2001) found a direct relationship between the occurrence of a
whale strike and the speed of the vessel involved in the collision. The
authors concluded that most deaths occurred when a vessel was traveling
in excess of 13 kts (24.1 km/hr, 14.9 mph).
NSF and ASC's proposed operation of one source vessel for the
proposed low-energy seismic survey is relatively small in scale
compared to the number of commercial ships transiting at higher speeds
in the same areas on an annual basis. The probability of vessel and
marine mammal interactions occurring during the proposed low-energy
seismic survey is unlikely due to the Palmer's slow operational speed,
which is typically 5 kts. Outside of seismic operations, the Palmer's
cruising speed would be approximately 10.1 to 14.5 kts, which is
generally below the speed at which studies have noted reported
increases of marine mammal injury or death (Laist et al., 2001).
As a final point, the Palmer has a number of other advantages for
avoiding ship strikes as compared to most commercial merchant vessels,
including the following: the Palmer's bridge and aloft observation
tower offers good visibility to visually monitor for marine mammal
presence; PSOs posted during operations scan the ocean for marine
mammals and must report visual alerts of marine mammal presence to
crew; and the PSOs receive extensive training that covers the
fundamentals of visual observing for marine mammals and information
about marine mammals and their identification at sea.
Entanglement
Entanglement can occur if wildlife becomes immobilized in survey
lines, cables, nets, or other equipment that is moving through the
water column. The proposed low-energy seismic survey would require
towing approximately a single 100 m cable streamer. This large of an
array carries the risk of entanglement for marine mammals. Wildlife,
especially slow moving individuals, such as large whales, have a low
probability of becoming entangled due to slow speed of the survey
vessel and onboard monitoring efforts. In May 2011, there was one
recorded entanglement of an olive ridley sea turtle (Lepidochelys
olivacea) in the R/V Marcus G. Langseth's barovanes after the
conclusion of a seismic survey off Costa Rica. There have been cases of
baleen whales, mostly gray whales (Heyning, 1990), becoming entangled
in fishing lines. The probability for entanglement of marine mammals is
considered not significant because of the vessel speed and the
monitoring efforts onboard the survey vessel.
Icebreaking Activities
Icebreakers produce more noise while breaking ice than ships of
comparable size due, primarily, to the sounds of propeller cavitating
(Richardson et al., 1995). Multi-year ice, which is expected to be
encountered in the proposed survey area. Icebreakers commonly back and
ram into heavy ice until losing momentum to make way. The highest noise
levels usually occur while backing full astern in preparation to ram
forward through the ice. Overall the noise generated by an icebreaker
pushing ice was 10 to 15 dB greater than the noise produced by the ship
underway in open water (Richardson et al., 1995). In general, the
Antarctic and Southern Ocean is a noisy environment. Calving and
grounding icebergs as well as the break-up of ice sheets, can produce a
large amount of underwater noise. Little information is available about
the increased sound levels due to icebreaking.
Cetaceans--Few studies have been conducted to evaluate the
potential interference of icebreaking noise with marine mammal
vocalizations. Erbe and Farmer (1998) measured masked hearing
thresholds of a captive beluga whale. They reported that the recording
of a CCG ship, Henry Larsen, ramming ice in the Beaufort Sea, masked
recordings of beluga vocalizations at a noise to signal pressure ratio
of 18 dB, when the noise pressure level was eight times as high as the
call pressure. Erbe and Farmer (2000) also predicted when icebreaker
noise would affect beluga whales through software that combined a sound
propagation model and beluga whale impact threshold models. They again
used the data from the recording of the Henry Larsen in the Beaufort
Sea and predicted that masking of beluga whale vocalizations could
extend between 40 and 71 km (21.6 and 38.3 nmi) near the surface.
Lesage et al. (1999) report that beluga whales changed their call type
and call frequency when exposed to boat noise. It is possible that the
whales adapt to the ambient noise levels and are able to communicate
despite the sound. Given the documented reaction of belugas to ships
and icebreakers it is highly unlikely that beluga whales would remain
in the proximity of vessels where vocalizations would be masked.
Beluga whales have been documented swimming rapidly away from ships
and icebreakers in the Canadian high Arctic when a ship approaches to
within 35 to 50 km (18.9 to 27 nmi), and they may travel up to 80 km
(43.2 nmi) from the vessel's track (Richardson et al., 1995). It is
expected that belugas avoid
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icebreakers as soon as they detect the ships (Cosens and Dueck, 1993).
However, the reactions of beluga whales to ships vary greatly and some
animals may become habituated to high levels of ambient noise (Erbe and
Darmber, 2000).
There is little information about the effects of icebreaking ships
on baleen whales. Migrating bowhead whales appeared to avoid an area
around a drill site by greater than 25 km (13.5 mi) where an icebreaker
was working in the Beaufort Sea. There was intensive icebreaking daily
in support of the drilling activities (Brewer et al., 1993). Migrating
bowheads also avoided a nearby drill site at the same time of year
where little icebreaking was being conducted (LGL and Greeneridge,
1987). It is unclear as to whether the drilling activities, icebreaking
operations, or the ice itself might have been the cause for the whale's
diversion. Bowhead whales are not expected to occur in the proximity of
the proposed action area.
Pinnipeds--Brueggeman et al. (1992) reported on the reactions of
seals to an icebreaker during activities at two prospects in the
Chukchi Sea. Reactions of seals to the icebreakers varied between the
two prospects. Most (67%) seals did not react to the icebreaker at
either prospect. Reaction at one prospect was greatest during
icebreaking activity (running/maneuvering/jogging) and was 0.23 km
(0.12 nmi) of the vessel and lowest for animals beyond 0.93 km (0.5
nmi). At the second prospect however, seal reaction was lowest during
icebreaking activity with higher and similar levels of response during
general (non-icebreaking) vessel operations and when the vessel was at
anchor or drifting. The frequency of seal reaction generally declined
with increasing distance from the vessel except during general vessel
activity where it remained consistently high to about 0.46 km (0.25
nmi) from the vessel before declining.
Similarly, Kanik et al. (1980) found that ringed (Pusa hispida) and
harp seals (Pagophilus groenlandicus) often dove into the water when an
icebreaker was breaking ice within 1 km (0.5 nmi) of the animals. Most
seals remained on the ice when the ship was breaking ice 1 to 2 km (0.5
to 1.1 nmi) away.
The potential effects to marine mammals described in this section
of the document do not take into consideration the proposed monitoring
and mitigation measures described later in this document (see the
``Proposed Mitigation'' and ``Proposed Monitoring and Reporting''
sections) which, as noted are designed to effect the least practicable
adverse impact on affected marine mammal species and stocks.
Anticipated Effects on Marine Mammal Habitat
The proposed seismic survey is not anticipated to have any
permanent impact on habitats used by the marine mammals in the proposed
survey area, including the food sources they use (i.e. fish and
invertebrates). Additionally, no physical damage to any habitat is
anticipated as a result of conducting airgun operations during the
proposed low-energy seismic survey. While it is anticipated that the
specified activity may result in marine mammals avoiding certain areas
due to temporary ensonification, this impact to habitat is temporary
and was considered in further detail earlier in this document, as
behavioral modification. The main impact associated with the proposed
activity will be temporarily elevated noise levels and the associated
direct effects on marine mammals in any particular area of the
approximately 5,628 km\2\ proposed project area, previously discussed
in this notice.
The Palmer is designed for continuous passage at 3 kts through ice
1 m thick. During the proposed project the Palmer will typically
encounter first- or second-year ice while avoiding thicker ice floes,
particularly large intact multi-year ice, whenever possible. In
addition, the vessel will follow leads when possible while following
the survey route. As the vessel passes through the ice, the ship causes
the ice to part and travel alongside the hull. This ice typically
returns to fill the wake as the ship passes. The effects are transitory
(i.e., hours at most) and localized (i.e., constrained to a relatively
narrow swath perhaps 10 m (32.1 ft) to each side of the vessel. The
Palmer's maximum beam is 18.3 m (60 ft). Applying the maximum estimated
amount of icebreaking (1,000 km), to the corridor opened by the ship,
NSF and ASC anticipate that a maximum of approximately 18 km\2\ (5.3
nmi\2\) of ice may be disturbed. This represents an inconsequential
amount of the total ice present in the Southern Ocean.
Sea ice is important for pinniped life functions such as resting,
breeding, and molting. Icebreaking activities may damage seal breathing
holes and will also reduce the haul-out area in the immediate vicinity
of the ship's track. Icebreaking along a maximum of 1,000 km of
trackline will alter local ice conditions in the immediate vicinity of
the vessel. This has the potential to temporarily lead to a reduction
of suitable seal haul-out habitat. However, the dynamic sea-ice
environment requires that seals be able to adapt to changes in sea,
ice, and snow conditions, and they therefore create new breathing holes
and lairs throughout the winter and spring (Hammill and Smith, 1989).
In addition, seals often use open leads and cracks in the ice to
surface and breathe (Smith and Stirling, 1975). Disturbance of the ice
will occur in a very small area relative to the Southern Ocean ice-pack
and no significant impact on marine mammals is anticipated by
icebreaking during the proposed low-energy seismic survey. The next
section discusses the potential impacts of anthropogenic sound sources
on common marine mammal prey in the proposed survey area (i.e., fish
and invertebrates).
Anticipated Effects on Fish
One reason for the adoption of airguns as the standard energy
source for marine seismic surveys is that, unlike explosives, they have
not been associated with large-scale fish kills. However, existing
information on the impacts of seismic surveys on marine fish and
invertebrate populations is limited. There are three types of potential
effects of exposure to seismic surveys: (1) Pathological, (2)
physiological, and (3) behavioral. Pathological effects involve lethal
and temporary or permanent sub-lethal injury. Physiological effects
involve temporary and permanent primary and secondary stress responses,
such as changes in levels of enzymes and proteins. Behavioral effects
refer to temporary and (if they occur) permanent changes in exhibited
behavior (e.g., startle and avoidance behavior). The three categories
are interrelated in complex ways. For example, it is possible that
certain physiological and behavioral changes could potentially lead to
an ultimate pathological effect on individuals (i.e., mortality).
The specific received sound levels at which permanent adverse
effects to fish potentially could occur are little studied and largely
unknown. Furthermore, the available information on the impacts of
seismic surveys on marine fish is from studies of individuals or
portions of a population; there have been no studies at the population
scale. The studies of individual fish have often been on caged fish
that were exposed to airgun pulses in situations not representative of
an actual seismic survey. Thus, available information provides limited
insight on possible real-world effects at the ocean or population
scale. This makes drawing conclusions about impacts on fish problematic
because, ultimately, the most important issues concern effects on
marine fish populations, their
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viability, and their availability to fisheries.
Hastings and Popper (2005), Popper (2009), and Popper and Hastings
(2009a, b) provided recent critical reviews of the known effects of
sound on fish. The following sections provide a general synopsis of the
available information on the effects of exposure to seismic and other
anthropogenic sound as relevant to fish. The information comprises
results from scientific studies of varying degrees of rigor plus some
anecdotal information. Some of the data sources may have serious
shortcomings in methods, analysis, interpretation, and reproducibility
that must be considered when interpreting their results (see Hastings
and Popper, 2005). Potential adverse effects of the program's sound
sources on marine fish are noted.
Pathological Effects--The potential for pathological damage to
hearing structures in fish depends on the energy level of the received
sound and the physiology and hearing capability of the species in
question. For a given sound to result in hearing loss, the sound must
exceed, by some substantial amount, the hearing threshold of the fish
for that sound (Popper, 2005). The consequences of temporary or
permanent hearing loss in individual fish on a fish population are
unknown; however, they likely depend on the number of individuals
affected and whether critical behaviors involving sound (e.g., predator
avoidance, prey capture, orientation and navigation, reproduction,
etc.) are adversely affected.
Little is known about the mechanisms and characteristics of damage
to fish that may be inflicted by exposure to seismic survey sounds. Few
data have been presented in the peer-reviewed scientific literature. As
far as NSF, ASC, and NMFS know, there are only two papers with proper
experimental methods, controls, and careful pathological investigation
implicating sounds produced by actual seismic survey airguns in causing
adverse anatomical effects. One such study indicated anatomical damage,
and the second indicated TTS in fish hearing. The anatomical case is
McCauley et al. (2003), who found that exposure to airgun sound caused
observable anatomical damage to the auditory maculae of pink snapper
(Pagrus auratus). This damage in the ears had not been repaired in fish
sacrificed and examined almost two months after exposure. On the other
hand, Popper et al. (2005) documented only TTS (as determined by
auditory brainstem response) in two of three fish species from the
Mackenzie River Delta. This study found that broad whitefish (Coregonus
nasus) exposed to five airgun shots were not significantly different
from those of controls. During both studies, the repetitive exposure to
sound was greater than would have occurred during a typical seismic
survey. However, the substantial low-frequency energy produced by the
airguns (less than 400 Hz in the study by McCauley et al. [2003] and
less than approximately 200 Hz in Popper et al. [2005]) likely did not
propagate to the fish because the water in the study areas was very
shallow (approximately nine m in the former case and less than two m in
the latter). Water depth sets a lower limit on the lowest sound
frequency that will propagate (the ``cutoff frequency'') at about one-
quarter wavelength (Urick, 1983; Rogers and Cox, 1988).
Wardle et al. (2001) suggested that in water, acute injury and
death of organisms exposed to seismic energy depends primarily on two
features of the sound source: (1) The received peak pressure, and (2)
the time required for the pressure to rise and decay. Generally, as
received pressure increases, the period for the pressure to rise and
decay decreases, and the chance of acute pathological effects
increases. According to Buchanan et al. (2004), for the types of
seismic airguns and arrays involved with the proposed program, the
pathological (mortality) zone for fish would be expected to be within a
few meters of the seismic source. Numerous other studies provide
examples of no fish mortality upon exposure to seismic sources (Falk
and Lawrence, 1973; Holliday et al., 1987; La Bella et al., 1996;
Santulli et al., 1999; McCauley et al., 2000a, b, 2003; Bjarti, 2002;
Thomsen, 2002; Hassel et al., 2003; Popper et al., 2005; Boeger et al.,
2006).
An experiment of the effects of a single 700 in\3\ airgun was
conducted in Lake Meade, Nevada (USGS, 1999). The data were used in an
Environmental Assessment of the effects of a marine reflection survey
of the Lake Meade fault system by the National Park Service (Paulson et
al., 1993, in USGS, 1999). The airgun was suspended 3.5 m (11.5 ft)
above a school of threadfin shad in Lake Meade and was fired three
successive times at a 30 second interval. Neither surface inspection
nor diver observations of the water column and bottom found any dead
fish.
For a proposed seismic survey in Southern California, USGS (1999)
conducted a review of the literature on the effects of airguns on fish
and fisheries. They reported a 1991 study of the Bay Area Fault system
from the continental shelf to the Sacramento River, using a 10 airgun
(5,828 in\3\) array. Brezzina and Associates were hired by USGS to
monitor the effects of the surveys and concluded that airgun operations
were not responsible for the death of any of the fish carcasses
observed. They also concluded that the airgun profiling did not appear
to alter the feeding behavior of sea lions, seals, or pelicans observed
feeding during the seismic surveys.
Some studies have reported, some equivocally, that mortality of
fish, fish eggs, or larvae can occur close to seismic sources
(Kostyuchenko, 1973; Dalen and Knutsen, 1986; Booman et al., 1996;
Dalen et al., 1996). Some of the reports claimed seismic effects from
treatments quite different from actual seismic survey sounds or even
reasonable surrogates. However, Payne et al. (2009) reported no
statistical differences in mortality/morbidity between control and
exposed groups of capelin eggs or monkfish larvae. Saetre and Ona
(1996) applied a `worst-case scenario' mathematical model to
investigate the effects of seismic energy on fish eggs and larvae. They
concluded that mortality rates caused by exposure to seismic surveys
are so low, as compared to natural mortality rates, that the impact of
seismic surveying on recruitment to a fish stock must be regarded as
insignificant.
Physiological Effects--Physiological effects refer to cellular and/
or biochemical responses of fish to acoustic stress. Such stress
potentially could affect fish populations by increasing mortality or
reducing reproductive success. Primary and secondary stress responses
of fish after exposure to seismic survey sound appear to be temporary
in all studies done to date (Sverdrup et al., 1994; Santulli et al.,
1999; McCauley et al., 2000a, b). The periods necessary for the
biochemical changes to return to normal are variable and depend on
numerous aspects of the biology of the species and of the sound
stimulus.
Behavioral Effects--Behavioral effects include changes in the
distribution, migration, mating, and catchability of fish populations.
Studies investigating the possible effects of sound (including seismic
survey sound) on fish behavior have been conducted on both uncaged and
caged individuals (e.g., Chapman and Hawkins, 1969; Pearson et al.,
1992; Santulli et al., 1999; Wardle et al., 2001; Hassel et al., 2003).
Typically, in these studies fish exhibited a sharp startle response at
the onset of a sound followed by habituation and a return to normal
behavior after the sound ceased.
[[Page 486]]
The Minerals Management Service (MMS, 2005) assessed the effects of
a proposed seismic survey in Cook Inlet. The seismic survey proposed
using three vessels, each towing two, four-airgun arrays ranging from
1,500 to 2,500 in\3\. MMS noted that the impact to fish populations in
the survey area and adjacent waters would likely be very low and
temporary. MMS also concluded that seismic surveys may displace the
pelagic fishes from the area temporarily when airguns are in use.
However, fishes displaced and avoiding the airgun noise are likely to
backfill the survey area in minutes to hours after cessation of seismic
testing. Fishes not dispersing from the airgun noise (e.g., demersal
species) may startle and move short distances to avoid airgun
emissions.
In general, any adverse effects on fish behavior or fisheries
attributable to seismic testing may depend on the species in question
and the nature of the fishery (season, duration, fishing method). They
may also depend on the age of the fish, its motivational state, its
size, and numerous other factors that are difficult, if not impossible,
to quantify at this point, given such limited data on effects of
airguns on fish, particularly under realistic at-sea conditions.
Anticipated Effects on Invertebrates
The existing body of information on the impacts of seismic survey
sound on marine invertebrates is very limited. However, there is some
unpublished and very limited evidence of the potential for adverse
effects on invertebrates, thereby justifying further discussion and
analysis of this issue. The three types of potential effects of
exposure to seismic surveys on marine invertebrates are pathological,
physiological, and behavioral. Based on the physical structure of their
sensory organs, marine invertebrates appear to be specialized to
respond to particle displacement components of an impinging sound field
and not to the pressure component (Popper et al., 2001).
The only information available on the impacts of seismic surveys on
marine invertebrates involves studies of individuals; there have been
no studies at the population scale. Thus, available information
provides limited insight on possible real-world effects at the regional
or ocean scale. The most important aspect of potential impacts concerns
how exposure to seismic survey sound ultimately affects invertebrate
populations and their viability, including availability to fisheries.
Literature reviews of the effects of seismic and other underwater
sound on invertebrates were provided by Moriyasu et al. (2004) and
Payne et al. (2008). The following sections provide a synopsis of
available information on the effects of exposure to seismic survey
sound on species of decapod crustaceans and cephalopods, the two
taxonomic groups of invertebrates on which most such studies have been
conducted. The available information is from studies with variable
degrees of scientific soundness and from anecdotal information. A more
detailed review of the literature on the effects of seismic survey
sound on invertebrates is provided in Appendix D of NSF/USGS's PEIS.
Pathological Effects--In water, lethal and sub-lethal injury to
organisms exposed to seismic survey sound appears to depend on at least
two features of the sound source: (1) The received peak pressure; and
(2) the time required for the pressure to rise and decay. Generally, as
received pressure increases, the period for the pressure to rise and
decay decreases, and the chance of acute pathological effects
increases. For the type of airgun array planned for the proposed
program, the pathological (mortality) zone for crustaceans and
cephalopods is expected to be within a few meters of the seismic
source, at most; however, very few specific data are available on
levels of seismic signals that might damage these animals. This premise
is based on the peak pressure and rise/decay time characteristics of
seismic airgun arrays currently in use around the world.
Some studies have suggested that seismic survey sound has a limited
pathological impact on early developmental stages of crustaceans
(Pearson et al., 1994; Christian et al., 2003; DFO, 2004). However, the
impacts appear to be either temporary or insignificant compared to what
occurs under natural conditions. Controlled field experiments on adult
crustaceans (Christian et al., 2003, 2004; DFO, 2004) and adult
cephalopods (McCauley et al., 2000a, b) exposed to seismic survey sound
have not resulted in any significant pathological impacts on the
animals. It has been suggested that exposure to commercial seismic
survey activities has injured giant squid (Guerra et al., 2004), but
the article provides little evidence to support this claim. Tenera
Environmental (2011b) reported that Norris and Mohl (1983, summarized
in Mariyasu et al., 2004) observed lethal effects in squid (Loligo
vulgaris) at levels of 246 to 252 dB after 3 to 11 minutes.
Andre et al. (2011) exposed four species of cephalopods (Loligo
vulgaris, Sepia officinalis, Octopus vulgaris, and Ilex coindetii),
primarily cuttlefish, to two hours of continuous 50 to 400 Hz
sinusoidal wave sweeps at 1575 dB re 1 [mu]Pa while captive
in relatively small tanks. They reported morphological and
ultrastructural evidence of massive acoustic trauma (i.e., permanent
and substantial alterations [lesions] of statocyst sensory hair cells)
to the exposed animals that increased in severity with time, suggesting
that cephalopods are particularly sensitive to low frequency sound. The
received SPL was reported as 1575 dB re 1 [mu]Pa, with peak
levels at 175 dB re 1 [mu]Pa. As in the McCauley et al. (2003) paper on
sensory hair cell damage in pink snapper as a result of exposure to
seismic sound, the cephalopods were subjected to higher sound levels
than they would be under natural conditions, and they were unable to
swim away from the sound source.
Physiological Effects--Physiological effects refer mainly to
biochemical responses by marine invertebrates to acoustic stress. Such
stress potentially could affect invertebrate populations by increasing
mortality or reducing reproductive success. Primary and secondary
stress responses (i.e., changes in haemolymph levels of enzymes,
proteins, etc.) of crustaceans have been noted several days or months
after exposure to seismic survey sounds (Payne et al., 2007). It was
noted however, than no behavioral impacts were exhibited by crustaceans
(Christian et al., 2003, 2004; DFO, 2004). The periods necessary for
these biochemical changes to return to normal are variable and depend
on numerous aspects of the biology of the species and of the sound
stimulus.
Behavioral Effects--There is increasing interest in assessing the
possible direct and indirect effects of seismic and other sounds on
invertebrate behavior, particularly in relation to the consequences for
fisheries. Changes in behavior could potentially affect such aspects as
reproductive success, distribution, susceptibility to predation, and
catchability by fisheries. Studies investigating the possible
behavioral effects of exposure to seismic survey sound on crustaceans
and cephalopods have been conducted on both uncaged and caged animals.
In some cases, invertebrates exhibited startle responses (e.g., squid
in McCauley et al., 2000a, b). In other cases, no behavioral impacts
were noted (e.g., crustaceans in Christian et al., 2003, 2004; DFO
2004). There have been anecdotal reports of
[[Page 487]]
reduced catch rates of shrimp shortly after exposure to seismic
surveys; however, other studies have not observed any significant
changes in shrimp catch rate (Andriguetto-Filho et al., 2005).
Similarly, Parry and Gason (2006) did not find any evidence that
lobster catch rates were affected by seismic surveys. Any adverse
effects on crustacean and cephalopod behavior or fisheries attributable
to seismic survey sound depend on the species in question and the
nature of the fishery (season, duration, fishing method).
Proposed Mitigation
In order to issue an Incidental Take Authorization (ITA) under
section 101(a)(5)(D) of the MMPA, NMFS must set forth the permissible
methods of taking pursuant to such activity, and other means of
effecting the least practicable impact on such species or stock and its
habitat, paying particular attention to rookeries, mating grounds, and
areas of similar significance, and the availability of such species or
stock for taking for certain subsistence uses.
NSF and ASC reviewed the following source documents and have
incorporated a suite of appropriate mitigation measures into their
project description.
(1) Protocols used during previous NSF and USGS-funded seismic
research cruises as approved by NMFS and detailed in the recently
completed ``Final Programmatic Environmental Impact Statement/Overseas
Environmental Impact Statement for Marine Seismic Research Funded by
the National Science Foundation or Conducted by the U.S. Geological
Survey;''
(2) Previous IHA applications and IHAs approved and authorized by
NMFS; and
(3) Recommended best practices in Richardson et al. (1995), Pierson
et al. (1998), and Weir and Dolman, (2007).
To reduce the potential for disturbance from acoustic stimuli
associated with the activities, NSF, ASC and/or its designees have
proposed to implement the following mitigation measures for marine
mammals:
(1) Proposed exclusion zones around the sound source;
(2) Speed and course alterations;
(3) Shut-down procedures; and
(4) Ramp-up procedures.
Proposed Exclusion Zones--During pre-planning of the cruise, the
smallest airgun array was identified that could be used and still meet
the geophysical scientific objectives. NSF and ASC use radii to
designate exclusion and buffer zones and to estimate take for marine
mammals. Table 2 (presented earlier in this document) shows the
distances at which one would expect to receive three sound levels (160,
180, and 190 dB) from the two GI airgun array. The 180 and 190 dB level
shut-down criteria are applicable to cetaceans and pinnipeds,
respectively, as specified by NMFS (2000). NSF and ASC used these
levels to establish the exclusion and buffer zones.
Received sound levels have been modeled by L-DEO for a number of
airgun configurations, including two 45 in\3\ Nucleus G airguns, in
relation to distance and direction from the airguns (see Figure 2 of
the IHA application). In addition, propagation measurements of pulses
from two GI airguns have been reported for shallow water (approximately
30 m [98.4 ft] depth in the GOM (Tolstoy et al., 2004). However,
measurements were not made for the two GI airguns in deep water. The
model does not allow for bottom interactions, and is most directly
applicable to deep water. Based on the modeling, estimates of the
maximum distances from the GI airguns where sound levels are predicted
to be 190, 180, and 160 dB re 1 [mu]Pa (rms) in shallow, intermediate,
and deep water were determined (see Table 2 above).
Empirical data concerning the 190, 180, and 160 dB (rms) distances
were acquired for various airgun arrays based on measurements during
the acoustic verification studies conducted by L-DEO in the northern
GOM in 2003 (Tolstoy et al., 2004) and 2007 to 2008 (Tolstoy et al.,
2009). Results of the 36 airgun array are not relevant for the two GI
airguns to be used in the proposed survey. The empirical data for the
6, 10, 12, and 20 airgun arrays indicate that, for deep water, the L-
DEO model tends to overestimate the received sound levels at a given
distance (Tolstoy et al., 2004). Measurements were not made for the two
GI airgun array in deep water; however, NSF and ASC propose to use the
safety radii predicted by L-DEO's model for the proposed GI airgun
operations in shallow, intermediate, and deep water, although they are
likely conservative given the empirical results for the other arrays.
Based on the modeling data, the outputs from the pair of 45 in\3\
or 105 in\3\ GI airguns proposed to be used during the seismic survey
are considered a low-energy acoustic source in the NSF/USGS PEIS (2011)
for marine seismic research. A low-energy seismic source was defined in
the NSF/USGS PEIS as an acoustic source whose received level at 100 m
is less than 180 dB. The NSF/USGS PEIS also established for these low-
energy sources, a standard exclusion zone of 100 m for all low-energy
sources in water depths greater than 100 m. This standard 100 m
exclusion zone would be used during the proposed low-energy seismic
survey. The 180 and 190 dB (rms) radii are shut-down criteria
applicable to cetaceans and pinnipeds, respectively, as specified by
NMFS (2000); these levels were used to establish exclusion zones.
Therefore, the assumed 180 and 190 dB radii are 100 m for intermediate
and deep water, respectively. If the PSO detects a marine mammal(s)
within or about to enter the appropriate exclusion zone, the airguns
will be shut-down immediately.
Speed and Course Alterations--If a marine mammal is detected
outside the exclusion zone and, based on its position and direction of
travel (relative motion), is likely to enter the exclusion zone,
changes of the vessel's speed and/or direct course will be considered
if this does not compromise operational safety or damage the deployed
equipment. This would be done if operationally practicable while
minimizing the effect on the planned science objectives. For marine
seismic surveys towing large streamer arrays, however, course
alterations are not typically implemented due to the vessel's limited
maneuverability. After any such speed and/or course alteration is
begun, the marine mammal activities and movements relative to the
seismic vessel will be closely monitored to ensure that the marine
mammal does not approach within the exclusion zone. If the marine
mammal appears likely to enter the exclusion zone, further mitigation
actions will be taken, including further speed and/or course
alterations, and/or shut-down of the airgun(s). Typically, during
seismic operations, the source vessel is unable to change speed or
course, and one or more alternative mitigation measures will need to be
implemented.
Shut-down Procedures--NSF and ASC will shut-down the operating
airgun(s) if a marine mammal is detected outside the exclusion zone for
the airgun(s), and if the vessel's speed and/or course cannot be
changed to avoid having the animal enter the exclusion zone, the
seismic source will be shut-down before the animal is within the
exclusion zone. Likewise, if a marine mammal is already within the
exclusion zone when first detected, the seismic source will be shut-
down immediately.
Following a shut-down, NSF and ASC will not resume airgun activity
until the marine mammal has cleared the exclusion zone. NSF and ASC
will consider the animal to have cleared the exclusion zone if:
[[Page 488]]
A PSO has visually observed the animal leave the exclusion
zone, or
A PSO has not sighted the animal within the exclusion zone
for 15 minutes for species with shorter dive durations (i.e., small
odontocetes and pinnipeds), or 30 minutes for species with longer dive
durations (i.e., mysticetes and large odontocetes, including sperm,
pygmy and dwarf sperm, killer, and beaked whales).
Although power-down procedures are often standard operating
practice for seismic surveys, they are not proposed to be used during
this planned seismic survey because powering-down from two airguns to
one airgun would make only a small difference in the exclusion
zone(s)--but probably not enough to allow continued one-airgun
operations if a marine mammal came within the exclusion zone for two
airguns.
Ramp-up Procedures--Ramp-up of an airgun array provides a gradual
increase in sound levels, and involves a step-wise increase in the
number and total volume of airguns firing until the full volume of the
airgun array is achieved. The purpose of a ramp-up is to ``warn''
marine mammals in the vicinity of the airguns and to provide the time
for them to leave the area avoiding any potential injury or impairment
of their hearing abilities. NSF and ASC will follow a ramp-up procedure
when the airgun array begins operating after a specified period without
airgun operations or when a shut-down shut down has exceeded that
period. NSF and ASC propose that, for the present cruise, this period
would be approximately 15 minutes. SIO, L-DEO, and USGS have used
similar periods (approximately 15 minutes) during previous low-energy
seismic surveys.
Ramp-up will begin with a single GI airgun (45 or 105 in\3\). The
second GI airgun (45 or 105 in\3\) will be added after 5 minutes.
During ramp-up, the PSOs will monitor the exclusion zone, and if marine
mammals are sighted, a shut-down will be implemented as though both GI
airguns were operational.
If the complete exclusion zone has not been visible for at least 30
minutes prior to the start of operations in either daylight or
nighttime, NSF and ASC will not commence the ramp-up. Given these
provisions, it is likely that the airgun array will not be ramped-up
from a complete shut-down at night or in thick fog, because the outer
part of the exclusion zone for that array will not be visible during
those conditions. If one airgun has operated, ramp-up to full power
will be permissible at night or in poor visibility, on the assumption
that marine mammals will be alerted to the approaching seismic vessel
by the sounds from the single airgun and could move away if they
choose. A ramp-up from a shut-down may occur at night, but only where
the exclusion zone is small enough to be visible. NSF and ASC will not
initiate a ramp-up of the airguns if a marine mammal is sighted within
or near the applicable exclusion zones during the day or close to the
vessel at night.
NMFS has carefully evaluated the applicant's proposed mitigation
measures and has considered a range of other measures in the context of
ensuring that NMFS prescribes the means of effecting the least
practicable adverse impact on the affected marine mammal species and
stocks and their habitat. NMFS's evaluation of potential measures
included consideration of the following factors in relation to one
another:
(1) The manner in which, and the degree to which, the successful
implementation of the measure is expected to minimize adverse impacts
to marine mammals;
(2) The proven or likely efficacy of the specific measure to
minimize adverse impacts as planned; and
(3) The practicability of the measure for applicant implementation.
Based on NMFS's evaluation of the applicant's proposed measures, as
well as other measures considered by NMFS or recommended by the public,
NMFS has preliminarily determined that the proposed mitigation measures
provide the means of effecting the least practicable adverse impacts on
marine mammal species or stocks and their habitat, paying particular
attention to rookeries, mating grounds, and areas of similar
significance.
Proposed Monitoring and Reporting
In order to issue an ITA for an activity, section 101(a)(5)(D) of
the MMPA states that NMFS must set forth ``requirements pertaining to
the monitoring and reporting of such taking.'' The MMPA implementing
regulations at 50 CFR 216.104 (a)(13) indicate that requests for IHAs
must include the suggested means of accomplishing the necessary
monitoring and reporting that will result in increased knowledge of the
species and of the level of taking or impacts on populations of marine
mammals that are expected to be present in the action area.
Proposed Monitoring
NSF and ASC proposes to sponsor marine mammal monitoring during the
proposed project, in order to implement the proposed mitigation
measures that require real-time monitoring, and to satisfy the
anticipated monitoring requirements of the IHA. NSF and ASC's proposed
``Monitoring Plan'' is described below this section. NSF and ASC
understand that this monitoring plan will be subject to review by NMFS
and that refinements may be required. The monitoring work described
here has been planned as a self-contained project independent of any
other related monitoring projects that may be occurring simultaneously
in the same regions. NSF and ASC is prepared to discuss coordination of
their monitoring program with any related work that might be done by
other groups insofar as this is practical and desirable.
Vessel-Based Visual Monitoring
PSOs will be based aboard the seismic source vessel and will watch
for marine mammals near the vessel during icebreaking activities,
daytime airgun operations (austral summer) and during any ramp-ups of
the airguns at night. Nighttime operations of the airguns are not
anticipated. PSOs will also watch for marine mammals near the seismic
vessel for at least 30 minutes prior to the start of airgun operations
and after an extended shut-down (i.e., greater than approximately 15
minutes for this proposed low-energy seismic survey). When feasible,
PSOs will conduct observations during daytime periods when the seismic
system is not operating (such as during transits) for comparison of
sighting rates and behavior with and without airgun operations and
between acquisition periods. Based on PSO observations, the airguns
will be shut-down when marine mammals are observed within or about to
enter a designated exclusion zone. The exclusion zone is a region in
which a possibility exists of adverse effects on animal hearing or
other physical effects.
During seismic operations in the Dumont d'Urville Sea of the
Southern Ocean, at least two PSOs will be based aboard the Palmer. At
least one PSO will stand watch at all times while the Palmer is
operating airguns during the proposed low-energy seismic survey; this
procedure will also be followed when the vessel is conducting
icebreaking during transit. NSF and ASC will appoint the PSOs with
NMFS's concurrence. The lead PSO would be experienced with marine
mammal species in the Southern Ocean, the second PSO would receive
additional specialized training from the PSO to ensure that they can
identify marine mammal species commonly found in the Southern Ocean.
Observations will take place during ongoing daytime operations and
nighttime ramp-ups of the airguns.
[[Page 489]]
During the majority of seismic operations, at least one PSO will be on
duty from observation platforms (i.e., the best available vantage point
on the source vessel) to monitor marine mammals near the seismic
vessel. PSO(s) will be on duty in shifts no longer than 4 hours in
duration. Other crew will also be instructed to assist in detecting
marine mammals and implementing mitigation requirements (if practical).
Before the start of the low-energy seismic survey, the crew will be
given additional instruction on how to do so. (Note: because of the
high latitude locations of the study areas, twilight/darkness
conditions are expected to be limited to between 3 and 6 hours per day
during the proposed action.)
The Palmer is a suitable platform for marine mammal observations
and will serve as the platform from which PSOs will watch for marine
mammals before and during seismic operations. Two locations are likely
as observation stations onboard the Palmer. Observing stations are
located on the bridge level, with the PSO eye level at approximately
16.5 m (54.1 ft) above the waterline and the PSO would have a good view
around the entire vessel. In addition, there is an aloft observation
tower for the PSO approximately 24.4 m (80.1 ft) above the waterline
that is protected from the weather, and affords PSOs an even greater
view. Standard equipment for PSOs will be reticle binoculars. Night-
vision equipment will not be available or required due to the constant
daylight conditions during the Antarctic summer. The PSOs will be in
communication with ship's officers on the bridge and scientists in the
vessel's operations laboratory, so they can advise promptly of the need
for avoidance maneuvers or seismic source shut-down. Observing stations
will be at the bridge level and the aloft observation tower. The
approximate view around the vessel from the bridge is 270[deg] and
360[deg] from the aloft observation tower. During daytime, the PSO(s)
will scan the area around the vessel systematically with reticle
binoculars (e.g., 7 x 50 Fujinon FMTRC-SX) and the naked eye. These
binoculars will have a built-in daylight compass. Estimating distances
is done primarily with the reticles in the binoculars. The PSO(s) will
be in direct (radio) wireless communication with ship's officers on the
bridge and scientists in the vessel's operations laboratory during
seismic operations, so they can advise the vessel operator, science
support personnel, and the science party promptly of the need for
avoidance maneuvers or a shut-down of the seismic source. PSOs will
monitor for the presence pinnipeds and cetaceans during icebreaking
activities, and will be limited to those marine mammal species in
proximity to the ice margin habitat. Observations within the buffer
zone would also include pinnipeds that may be present on the surface of
the sea ice (i.e., hauled-out) and that could potentially dive into the
water as the vessel approaches, indicating disturbance from noise
generated by icebreaking activities).
When marine mammals are detected within or about to enter the
designated exclusion zone, the airguns will immediately be shut-down if
necessary. The PSO(s) will continue to maintain watch to determine when
the animal(s) are outside the exclusion zone by visual confirmation.
Airgun operations will not resume until the animal is confirmed to have
left the exclusion zone, or if not observed after 15 minutes for
species with shorter dive durations (small odontocetes and pinnipeds)
or 30 minutes for species with longer dive durations (mysticetes and
large odontocetes, including sperm, killer, and beaked whales).
PSO Data and Documentation
PSOs will record data to estimate the numbers of marine mammals
exposed to various received sound levels and to document apparent
disturbance reactions or lack thereof. Data will be used to estimate
numbers of animals potentially ``taken'' by harassment (as defined in
the MMPA). They will also provide information needed to order a shut-
down of the airguns when a marine mammal is within or near the
exclusion zone. Observations will also be made during icebreaking
activities as well as daytime periods when the Palmer is underway
without seismic operations (i.e., transits, to, from, and through the
study area) to collect baseline biological data.
When a sighting is made, the following information about the
sighting will be recorded:
1. Species, group size, age/size/sex categories (if determinable),
behavior when first sighted and after initial sighting, heading (if
consistent), bearing and distance from seismic vessel, sighting cue,
apparent reaction to the seismic source or vessel (e.g., none,
avoidance, approach, paralleling, etc.), and behavioral pace.
2. Time, location, heading, speed, activity of the vessel, sea
state, wind force, visibility, and sun glare.
The data listed under (2) will also be recorded at the start and
end of each observation watch, and during a watch whenever there is a
change in one or more of the variables.
All observations, as well as information regarding ramp-ups or
shut-downs will be recorded in a standardized format. Data will be
entered into an electronic database. The data accuracy will be verified
by computerized data validity checks as the data are entered and by
subsequent manual checking of the database by the PSOs at sea. These
procedures will allow initial summaries of data to be prepared during
and shortly after the field program, and will facilitate transfer of
the data to statistical, graphical, and other programs for further
processing and archiving.
Results from the vessel-based observations will provide the
following information:
1. The basis for real-time mitigation (airgun shut-down).
2. Information needed to estimate the number of marine mammals
potentially taken by harassment, which must be reported to NMFS.
3. Data on the occurrence, distribution, and activities of marine
mammals in the area where the seismic study is conducted.
4. Information to compare the distance and distribution of marine
mammals relative to the source vessel at times with and without seismic
activity.
5. Data on the behavior and movement patterns of marine mammals
seen at times with and without seismic activity.
NSF and ASC will submit a comprehensive report to NMFS within 90
days after the end of the cruise. The report will describe the
operations that were conducted and sightings of marine mammals near the
operations. The report submitted to NMFS will provide full
documentation of methods, results, and interpretation pertaining to all
monitoring. The 90-day report will summarize the dates and locations of
seismic operations and all marine mammal sightings (i.e., dates, times,
locations, activities, and associated seismic survey activities). The
report will minimally include:
Summaries of monitoring effort--total hours, total
distances, and distribution of marine mammals through the study period
accounting for Beaufort sea state and other factors affecting
visibility and detectability of marine mammals;
Analyses of the effects of various factors influencing
detectability of marine mammals including Beaufort sea state, number of
PSOs, and fog/glare;
Species composition, occurrence, and distribution of
marine mammals sightings including date, water depth,
[[Page 490]]
numbers, age/size/gender, and group sizes; and analyses of the effects
of seismic operations;
Sighting rates of marine mammals during periods with and
without airgun activities (and other variables that could affect
detectability);
Initial sighting distances versus airgun activity state;
Closest point of approach versus airgun activity state;
Observed behaviors and types of movements versus airgun
activity state;
Numbers of sightings/individuals seen versus airgun
activity state; and
Distribution around the source vessel versus airgun
activity state.
The report will also include estimates of the number and nature of
exposures that could result in ``takes'' of marine mammals by
harassment or in other ways. After the report is considered final, it
will be publicly available on the NMFS Web site at: https://www.nmfs.noaa.gov/pr/permits/incidental.htm#iha.
In the unanticipated event that the specified activity clearly
causes the take of a marine mammal in a manner prohibited by this IHA,
such as an injury (Level A harassment), serious injury or mortality
(e.g., ship-strike, gear interaction, and/or entanglement), NSF and ASC
will immediately cease the specified activities and immediately report
the incident to the Chief of the Permits and Conservation Division,
Office of Protected Resources, NMFS at 301-427-8401 and/or by email to
Jolie.Harrison@noaa.gov and Howard.Goldstein@noaa.gov. The report must
include the following information:
Time, date, and location (latitude/longitude) of the
incident;
Name and type of vessel involved;
Vessel's speed during and leading up to the incident;
Description of the incident;
Status of all sound source use in the 24 hours preceding
the incident;
Water depth;
Environmental conditions (e.g., wind speed and direction,
Beaufort sea state, cloud cover, and visibility);
Description of all marine mammal observations in the 24
hours preceding the incident;
Species identification or description of the animal(s)
involved;
Fate of the animal(s); and
Photographs or video footage of the animal(s) (if
equipment is available).
Activities shall not resume until NMFS is able to review the
circumstances of the prohibited take. NMFS shall work with NSF and ASC
to determine what is necessary to minimize the likelihood of further
prohibited take and ensure MMPA compliance. NSF and ASC may not resume
their activities until notified by NMFS via letter or email, or
telephone.
In the event that NSF and ASC discovers an injured or dead marine
mammal, and the lead PSO determines that the cause of the injury or
death is unknown and the death is relatively recent (i.e., in less than
a moderate state of decomposition as described in the next paragraph),
NSF and ASC will immediately report the incident to the Chief of the
Permits and Conservation Division, Office of Protected Resources, NMFS,
at 301-427-8401, and/or by email to Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report must include the same information
identified in the paragraph above. Activities may continue while NMFS
reviews the circumstances of the incident. NMFS will work with NSF and
ASC to determine whether modifications in the activities are
appropriate.
In the event that NSF and ASC discovers an injured or dead marine
mammal, and the lead PSO determines that the injury or death is not
associated with or related to the activities authorized in the IHA
(e.g., previously wounded animal, carcass with moderate or advanced
decomposition, or scavenger damage), NSF and ASC will report the
incident to the Chief of the Permits and Conservation Division, Office
of Protected Resources, NMFS, at 301-427-8401, and/or by email to
Jolie.Harrison@noaa.gov and Howard.Goldstein@noaa.gov, within 24 hours
of discovery. NSF and ASC will provide photographs or video footage (if
available) or other documentation of the stranded animal sighting to
NMFS. Activities may continue while NMFS reviews the circumstances of
the incident.
Estimated Take by Incidental Harassment
Except with respect to certain activities not pertinent here, the
MMPA defines ``harassment'' as: any act of pursuit, torment, or
annoyance which (i) has the potential to injure a marine mammal or
marine mammal stock in the wild [Level A harassment]; or (ii) has the
potential to disturb a marine mammal or marine mammal stock in the wild
by causing disruption of behavioral patterns, including, but not
limited to, migration, breathing, nursing, breeding, feeding, or
sheltering [Level B harassment].
Level B harassment is anticipated and proposed to be authorized as
a result of the proposed low-energy marine seismic survey in the Dumont
d'Urville Sea off the coast of East Antarctica. Acoustic stimuli (i.e.,
increased underwater sound) generated during the operation of the
seismic airgun array and icebreaking activities are expected to result
in the behavioral disturbance of some marine mammals. There is no
evidence that the planned activities could result in injury, serious
injury, or mortality for which NSF and ASC seeks the IHA. The required
mitigation and monitoring measures will minimize any potential risk for
injury, serious injury, or mortality.
The following sections describe NSF and ASC's methods to estimate
take by incidental harassment and present the applicant's estimates of
the numbers of marine mammals that could be affected during the
proposed low-energy seismic survey in the Dumont d'Urville Sea off the
coast of East Antarctica. The estimates are based on a consideration of
the number of marine mammals that could be harassed by approximately
2,800 km (1511.9 nmi) of seismic operations with the two GI airgun
array to be used and 1,000 km of icebreaking activities.
During simultaneous operations of the airgun array and the other
sound sources, any marine mammals close enough to be affected by the
single and multi-beam echosounders, pingers, ADCP, sub-bottom profiler,
etc. would already be affected by the airguns. During times when the
airguns are not operating, it is unlikely that marine mammals will
exhibit more than minor, short-term responses to the echosounders,
ADCPs, and sub-bottom profiler given their characteristics (e.g.,
narrow, downward-directed beam) and other considerations described
previously. Therefore, for this activity, take was not authorized
specifically for these sound sources beyond that which is already
authorized for airguns and icebreaking activities.
There are no stock assessments and very limited population
information available for marine mammals in the Dumont d'Urville Sea.
Sighting data from the Australian Antarctic Division's (AAD) BROKE-West
surveys (Southwell et al., 2008; 2012) was used to determine and
estimate marine mammals densities for mysticetes and odontocetes and
AAD data components for pinnipeds, which were not available for the
proposed seismic survey's action area in the Dumont d'Urville Sea.
While population density data for cetaceans in the Southern Ocean is
sparse to nonexistent, reported sightings data from previous research
cruises suggest cetaceans such as those identified in Table 12 of the
IHA application span a range greater than 4,000 km (2,159.8 nmi) off
the coast of East Antarctica.
[[Page 491]]
The AAD BROKE-West survey was not specifically designed to quantify
marine mammals. The data was in terms of animals sighted per time unit,
and this sighting data was then converted to an areal density by
multiplying the number of animals observed by the estimated area
observed during the survey. As such, some marine mammals that were
present in the area may not have been observed.
The estimated number of cetaceans and pinnipeds that may be
potentially exposed from the proposed seismic airgun operations and
icebreaking activities based on sighting data from previous research
cruises over a 52-day period and 13-day period. Some of the AAD
sighting data was used as the basis for estimating take included
``unidentified whale'' species, this category was retained and pro-
rated to the other species because environmental conditions may be
present during the proposed action to limit identification of observed
cetaceans. The estimated frequency of sightings data for cetaceans
incorporates a correction factor of 5 that assumes only 20% of the
animals present were reported due to sea ice and other conditions that
may have hindered observation. The 20% factor was intended to
conservatively account for this. Conservatively, a 40% correction
factor was used for pinnipeds. The expected sightings data incorporates
a 40% correction factor to account for seals that may be in the water
versus those hauled-out on ice surface. This correction factor for
pinnipeds was conservatively based on Southwell et al. (2012), which
estimated 20 to 40% of crabeater seals may be in the water in a
particular area while the rest are hauled-out. The correction factor
takes into consideration some pinnipeds may not be observed due to poor
visibility conditions.
Sightings data were collected by the AAD; however, the AAD
methodology was not described. Density is generally reported in the
number of animals per km or square km. Estimated area observed by
observers was calculated by using the average vessel speed (5.6 km/hr)
times the estimated hours of the survey to estimate the total distance
covered for each of the surveys. This was then converted from the
linear distance into an area by assuming a width of 5 km that could be
reliably visually surveyed. Therefore, the estimated area was 5,753
km\2\ (1,677.3 nmi\2\) to obtain mysticete and odontocete densities and
the estimated area was 1,419 km\2\ (413.7 nmi\2\) to obtain pinniped
densities.
Of the six species of pinnipeds that may be present in the study
area during the proposed action, only four species are expected to be
observed and occur mostly near pack ice or coastal areas and not
prevalent in open sea areas where the low-energy seismic survey would
be conducted. Because density estimates for pinnipeds in that Antarctic
regions typically represent individuals that have hauled-out of the
water, those estimates are not representative of individuals that are
in the water and could be potentially exposed to underwater sounds
during the seismic airgun operations and icebreaking activities;
therefore, the pinniped densities have been adjusted to account for
this concern. Take was not requested for southern elephant seals and
Antarctic fur seals because preferred habitat for these species is not
within the proposed action area. Although no sightings of Weddell seals
and spectacled porpoises were reported in the BROKE-West sighting data,
take was requested for these species based on NMFS recommendation and
IWC SOWER data. Although there is some uncertainty about the
representatives of the data and the assumptions used in the
calculations below, the approach used here is believed to be the best
available approach.
Table 5. Estimated densities and possible number of marine mammal
species that might be exposed to greater than or equal to 120 dB
(icebreaking) and 160 dB (airgun operations) during NSF and ASC's
proposed low-energy seismic survey (approximately 1,000 km of
tracklines/approximately 3,500 km\2\ ensonified area for icebreaking
activities and approximately 2,800 km of tracklines/approximately 5,628
km\2\ ensonified area for airgun operations) in the Dumont d'Urville
Sea of the Southern Ocean, February to March 2014.
--------------------------------------------------------------------------------------------------------------------------------------------------------
Calculated Calculated
take from take from
Reported seismic airgun icebreaking
sightings 1 2 Corrected Density in- operations activities Approximate
*sightings sightings water [density (i.e., (i.e., percentage of
have been pro- (assume 20% in-water and/ estimated estimated population Total requested take
Species rated to for cetaceans, or on-ice] number of number of estimate authorization \6\
include 40% of (/km) individuals individuals (calculated
unidentified pinnipeds in \2\ exposed to exposed to total take)
animals* water) sound levels sound levels \5\
>=160 dB re 1 >=120 dB re 1
[mu]Pa) \3\ [mu]Pa) \4\
--------------------------------------------------------------------------------------------------------------------------------------------------------
Mysticetes:
Southern right whale.... 0 0 0 0 0 NA 0.
Humpback whale.......... 238 1,190 0.2068400 1,165 724 5.4 1,165 + 724 = 1,889.
Antarctic minke whale... 136 680 0.1181943 666 414 0.4 666 + 414 = 1,080.
Sei whale............... 4 20 0.0034763 20 13 0.04 20 + 13 = 33.
Fin whale............... 232 1,160 0.2016255 1,135 706 1.3 1,135 + 706 = 1,841.
Blue whale.............. 2 10 0.0017382 10 7 1.0 10 + 7 = 17.
Odontocetes:
Sperm whale............. 32 160 0.0278104 157 98 2.7 157 + 98 = 255.
Arnoux's beaked whale... 0 0 0 0 0 NA 0.
Cuvier's beaked whale... 0 0 0 0 0 NA 0.
Southern bottlenose 0 0 0 0 0 NA 0.
beaked whale.
Killer whale............ 62 310 0.538827 304 189 2.0 304 + 189 = 493.
Long-finned pilot whale. 24 120 0.0208578 118 74 0.1 118 + 74 = 192.
Hourglass dolphin....... 27 135 0.0234650 133 83 0.15 133 + 83 = 216.
Spectacled porpoise..... 26 130 0.0225690 128 80 NA 128 + 80 = 208.
Pinnipeds:
Crabeater seal.......... 2,220 888 0.625546 3,521 7,663 0.2 3,521 + 7,663 = 11,184.
[2.189411]
Leopard seal............ 17 7 0.00479 27 59 0.04 27 + 59 = 86.
[0.016766]
Ross seal............... 42 17 0.011835 66 145 0.2 66 + 145 = 211.
[0.041421]
[[Page 492]]
Weddell seal............ 302 121 0.054 303 189 0.1 303 + 189 = 492.
[0.054]
Southern elephant seal.. 0 0 0 0 0 NA 0.
Antarctic fur seal...... 0 0 0 0 0 NA 0.
--------------------------------------------------------------------------------------------------------------------------------------------------------
NA = Not available or not assessed.
\1\ Sightings from a 52 day (5,753 km\2\) period on the AAD BROKE-West survey during January to March 2006.
\2\ Sightings December 3 to 16, 1999 (1,420 km\2\ and 75,564 km\2\), below 60[deg] South latitude between 110 to 165[deg] East longitude. All sightings
were animals hauled-out of the water and on the sea ice.
\3\ Calculated take is estimated density (reported density times correction factor) multiplied by the area ensonified to 160 dB (rms) around the planned
seismic lines, increased by 25% for contingency.
\4\ Calculated take is estimated density (reported density) multiplied by the area ensonified to 120 dB (rms) around the planned transit lines where
icebreaking activities may occur.
\5\ Total requested (and calculated) takes expressed as percentages of the species or regional populations.
\6\ Requested Take Authorization includes unidentified animals that were added to the observed and identified species on a pro-rated basis.
Note: Take was not requested for southern elephant seals and Antarctic fur seals because preferred habitat for these species is not within the proposed
action area.
Icebreaking in Antarctic waters will occur, as necessary, between
the latitudes of approximately 66 to 70[deg] South and between 140 and
165[deg] East. Based on a maximum sea ice extent of 250 km and
estimating that the Palmer will transit to the innermost shelf and back
into open water twice--a round trip transit in each of the potential
work regions, it is estimated that the Palmer will actively break ice
up to a distance of 1,000 km. Based on the ship's speed of 5 kts under
moderate ice conditions, this distance represents approximately 108 hrs
of icebreaking operations. This calculation is likely an overestimation
because icebreakers often follow leads when they are available and thus
do not break ice at all times.
Numbers of marine mammals that might be present and potentially
disturbed are estimated based on the available data about marine mammal
distribution and densities in the Southern Ocean study are during the
austral summer. NSF and ASC estimated the number of different
individuals that may be exposed to airgun sounds with received levels
greater than or equal to 160 dB re 1 [mu]Pa (rms) for seismic airgun
operations and greater than or equal to 120 dB re 1 [mu]Pa (rms) for
icebreaking activities on one or more occasions by considering the
total marine area that would be within the 160 dB radius around the
operating airgun array and 120 dB radius for the icebreaking activities
on at least one occasion and the expected density of marine mammals in
the area (in the absence of the a seismic survey and icebreaking
activities). The number of possible exposures can be estimated by
considering the total marine area that would be within the 160 dB
radius (i.e., diameter is 1,005 m times 2) around the operating
airguns. The ensonified area for icebreaking was estimated by
multiplying the distance of the icebreaking activities (1,000 km) by
the estimated diameter of the area within the 120 dB radius (i.e.,
diameter is 1,750 m times 2). The 160 dB radii are based on acoustic
modeling data for the airguns that may be used during the proposed
action (see Attachment B of the IHA application). As summarized in
Table 2 (see Table 11 of the IHA application), the modeling results for
the proposed low-energy seismic airgun array indicate the received
levels are dependent on water depth. Since the majority of the proposed
airgun operations would be conducted in waters 100 to 1,000 m deep, the
buffer zone of 1,005 m used for the two 105 in\3\ GI airguns was used
to be more conservative. The expected sighting data for pinnipeds
accounts for both pinnipeds that may be in the water and those hauled-
out on ice surfaces. While the number of cetaceans that may be
encountered within the ice margin habitat would be expected to be less
than open water, the estimates utilized expected sightings for the open
water and represent conservative estimates. It is unlikely that a
particular animal would stay in the area during the entire survey.
The number of different individuals potentially exposed to received
levels greater than or equal to 160 dB re 1 [mu]Pa (rms) from seismic
airgun operations and 120 dB re 1 [mu]Pa (rms) for icebreaking
activities was calculated by multiplying:
(1) The expected species density (in number/km\2\), times.
(2) The anticipated area to be ensonified to that level during
airgun operations.
Applying the approach described above, approximately 5,628 km\2\
(including the 25% contingency) would be ensonified within the 160 dB
isopleth for seismic airgun operations and approximately 3,500 km\2\
would be ensonified within the 120 dB isopleth for icebreaking
activities on one or more occasions during the proposed survey. The
take calculations within the study sites do not explicitly add animals
to account for the fact that new animals (i.e., turnover) are not
accounted for in the initial density snapshot and animals could also
approach and enter the area ensonified above 160 dB for seismic airgun
operations and 120 dB for icebreaking activities; however, studies
suggest that many marine mammals will avoid exposing themselves to
sounds at this level, which suggests that there would not necessarily
be a large number of new animals entering the area once the seismic
survey and icebreaking activities started. Because this approach for
calculating take estimates does not allow for turnover in the marine
mammal populations in the area during the course of the survey, the
actual number of individuals exposed may be underestimated, although
the conservative (i.e., probably overestimated) line-kilometer
distances used to calculate the area may offset this. Also, the
approach assumes that no cetaceans or pinnipeds will move away or
toward the tracklines as the Palmer approaches in response to
increasing sound levels before the levels reach 160 dB for seismic
airgun operations and 120 dB for icebreaking activities. Another way of
interpreting the
[[Page 493]]
estimates that follow is that they represent the number of individuals
that are expected (in absence of a seismic and icebreaking program) to
occur in the waters that will be exposed to greater than or equal to
160 dB (rms) for seismic airgun operations and greater than or equal to
120 dB (rms) for icebreaking activities.
NSF and ASC's estimates of exposures to various sound levels assume
that the proposed surveys will be carried out in full; however, the
ensonified areas calculated using the planned number of line-kilometers
has been increased by 25% to accommodate lines that may need to be
repeated, equipment testing, etc. As is typical during offshore ship
surveys, inclement weather and equipment malfunctions are likely to
cause delays and may limit the number of useful line-kilometers of
seismic operations that can be undertaken. The estimates of the numbers
of marine mammals potentially exposed to 120 dB (rms) and 160 dB (rms)
received levels are precautionary and probably overestimate the actual
numbers of marine mammals that could be involved. These estimates
assume that there will be no weather, equipment, or mitigation delays,
which is highly unlikely.
Table 5 shows the estimates of the number of different individual
marine mammals anticipated to be exposed to greater than or equal to
120 dB re 1 [mu]Pa (rms) for icebreaking activities and greater than or
equal to 160 dB re 1 [mu]Pa (rms) for seismic airgun operations during
the seismic survey if no animals moved away from the survey vessel. The
total requested take authorization is given in the far right column of
Table 5.
The estimate of the number of individual cetaceans and pinnipeds
that could be exposed to seismic sounds with received levels greater
than or equal to 160 dB re 1 [mu]Pa (rms) and sounds from icebreaking
activities with received levels greater than or equal to 120 dB re 1
[mu]Pa (rms) during the proposed survey is (with 25% contingency) in
Table 5 of this document. That total (with 25% contingency) includes
1,889 humpback, 1,080 Antarctic minke, 33 sei, 1,841 fin, 17 blue, and
255 sperm whales could be taken by Level B harassment during the
proposed seismic survey, which would represent 5.4, 0.4, 0.04, 1.3, 1,
and 2.7% of the worldwide or regional populations, respectively. Some
of the cetaceans potentially taken by Level B harassment are delphinids
and porpoises: killer whales, long-finned pilot whales, hourglass
dolphins, and spectacled porpoises are estimated to be the most common
delphinid and porpoise species in the area, with estimates of 493, 192,
216, and 208, which would represent 2, 0.1, and 0.15% (spectacled
porpoise population is not available) of the affected worldwide or
regional populations, respectively. Most of the pinnipeds potentially
taken by Level B harassment are: Crabeater, leopard, Ross, and Weddell
seals with estimates of 11,184, 86, 211, and 492, which would represent
0.2, 0.04, 0.2, and 0.1% of the affected worldwide or regional
populations, respectively.
Encouraging and Coordinating Research
NSF and ASC will coordinate the planned marine mammal monitoring
program associated with the proposed low-energy seismic survey with
other parties that express interest in this activity and area. NSF and
ASC will coordinate with applicable U.S. agencies (e.g., NMFS), and
will comply with their requirements. NSF has already reached out to the
Australian Antarctic Division (AAD), who are the proponents of the
proposed marine protected area and regularly conduct research
expeditions in the marine environment off East Antarctica.
The proposed action would complement fieldwork studying other
Antarctic ice shelves, oceanographic studies, and ongoing development
of ice sheet and other ocean models. It would facilitate learning at
sea and ashore by students, help to fill important spatial and temporal
gaps in a lightly sampled region of coastal Antarctica, provide
additional data on marine mammals present in the East Antarctic study
areas, and communicate its findings via reports, publications and
public outreach.
Impact on Availability of Affected Species or Stock for Taking for
Subsistence Uses
Section 101(a)(5)(D) of the MMPA also requires NMFS to determine
that the authorization will not have an unmitigable adverse effect on
the availability of marine mammal species or stocks for subsistence
use. There are no relevant subsistence uses of marine mammals in the
study area (in the Dumont d'Urville Sea off the coast of East
Antarctica) that implicate MMPA section 101(a)(5)(D).
Negligible Impact and Small Numbers Analysis Determination
As a preliminary matter, NMFS typically includes our negligible
impact and small numbers analyses and determinations under the same
section heading of our Federal Register notices. Despite co-locating
these terms, NMFS acknowledges that negligible impact and small numbers
are distinct standards under the MMPA and treat them as such. The
analyses presented below do not conflate the two standards; instead,
each standard has been considered independently and NMFS has applied
the relevant factors to inform our negligible impact and small numbers
determinations.
NMFS has defined ``negligible impact'' in 50 CFR 216.103 as ``an
impact resulting from the specified activity that cannot be reasonably
expected to, and is not reasonably likely to, adversely affect the
species or stock through effects on annual rates of recruitment or
survival.'' In making a negligible impact determination, NMFS evaluated
factors such as:
(1) The number of anticipated injuries, serious injuries, or
mortalities;
(2) The number, nature, and intensity, and duration of Level B
harassment (all relatively limited); and
(3) The context in which the takes occur (i.e., impacts to areas of
significance, impacts to local populations, and cumulative impacts when
taking into account successive/contemporaneous actions when added to
baseline data);
(4) The status of stock or species of marine mammals (i.e.,
depleted, not depleted, decreasing, increasing, stable, impact relative
to the size of the population);
(5) Impacts on habitat affecting rates of recruitment/survival; and
(6) The effectiveness of monitoring and mitigation measures.
As described above and based on the following factors, the
specified activities associated with the marine seismic survey are not
likely to cause PTS, or other non-auditory injury, serious injury, or
death. The factors include:
(1) The likelihood that, given sufficient notice through relatively
slow ship speed, marine mammals are expected to move away from a noise
source that is annoying prior to its becoming potentially injurious;
(2) The potential for temporary or permanent hearing impairment is
relatively low and would likely be avoided through the implementation
of the shut-down measures;
No injuries, serious injuries, or mortalities are anticipated to
occur as a result of the NSF and ASC's planned low-energy marine
seismic survey, and none are proposed to be authorized by NMFS. Table 5
of this document outlines the number of requested Level B harassment
takes that are anticipated as a result of these activities. Due to the
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nature, degree, and context of Level B (behavioral) harassment
anticipated and described (see ``Potential Effects on Marine Mammals''
section above) in this notice, the activity is not expected to impact
rates of annual recruitment or survival for any affected species or
stock, particularly given NMFS's and the applicant's proposal to
implement mitigation, monitoring, and reporting measures to minimize
impacts to marine mammals. Additionally, the seismic survey will not
adversely impact marine mammal habitat.
For the other marine mammal species that may occur within the
proposed action area, there are no known designated or important
feeding and/or reproductive areas. Many animals perform vital
functions, such as feeding, resting, traveling, and socializing, on a
diel cycle (i.e., 24 hr cycle). Behavioral reactions to noise exposure
(such as disruption of critical life functions, displacement, or
avoidance of important habitat) are more likely to be significant if
they last more than one diel cycle or recur on subsequent days
(Southall et al., 2007). Additionally, the seismic survey will be
increasing sound levels in the marine environment in a relatively small
area surrounding the vessel (compared to the range of the animals),
which is constantly travelling over distances, and some animals may
only be exposed to and harassed by sound for less than day.
Of the 14 marine mammal species under NMFS jurisdiction that may or
are known to likely to occur in the study area, five are listed as
threatened or endangered under the ESA: southern right, humpback, sei,
fin, blue, and sperm whales. These species are also considered depleted
under the MMPA. Of these ESA-listed species, incidental take has been
requested to be authorized for humpback, sei, fin, blue, and sperm
whales. There is generally insufficient data to determine population
trends for the other depleted species in the study area. To protect
these animals (and other marine mammals in the study area), NSF and ASC
must cease or reduce airgun operations if any marine mammal enters
designated zones. No injury, serious injury, or mortality is expected
to occur and due to the nature, degree, and context of the Level B
harassment anticipated, and the activity is not expected to impact
rates of recruitment or survival.
As mentioned previously, NMFS estimates that 14 species of marine
mammals under its jurisdiction could be potentially affected by Level B
harassment over the course of the IHA. The population estimates for the
marine mammal species that may be taken by Level B harassment were
provided in Table 4 of this document.
NMFS's practice has been to apply the 160 dB re 1 [mu]Pa (rms)
received level threshold for underwater impulse sound levels and the
120 dB re 1 [mu]Pa (rms) received level threshold for icebreaking
activities to determine whether take by Level B harassment occurs.
Southall et al. (2007) provide a severity scale for ranking observed
behavioral responses of both free-ranging marine mammals and laboratory
subjects to various types of anthropogenic sound (see Table 4 in
Southall et al. [2007]).
NMFS has preliminarily determined, provided that the aforementioned
mitigation and monitoring measures are implemented, the impact of
conducting a low-energy marine seismic survey in the Dumont d'Urville
Sea off the coast of East Antarctica, February to March 2014, may
result, at worst, in a modification in behavior and/or low-level
physiological effects (Level B harassment) of certain species of marine
mammals.
While behavioral modifications, including temporarily vacating the
area during the operation of the airgun(s), may be made by these
species to avoid the resultant acoustic disturbance, the availability
of alternate areas within these areas for species and the short and
sporadic duration of the research activities, have led NMFS to
preliminary determine that the taking by Level B harassment from the
specified activity will have a negligible impact on the affected
species in the specified geographic region. NMFS believes that the
length of the seismic survey, the requirement to implement mitigation
measures (e.g., shut-down of seismic operations), and the inclusion of
the monitoring and reporting measures, will reduce the amount and
severity of the potential impacts from the activity to the degree that
it will have a negligible impact on the species or stocks in the action
area.
NMFS has preliminary determined, provided that the aforementioned
mitigation and monitoring measures are implemented, that the impact of
conducting a low-energy marine seismic survey in the Dumont d'Urville
Sea off the coast of East Antarctica, January to March 2014, may
result, at worst, in a temporary modification in behavior and/or low-
level physiological effects (Level B harassment) of small numbers of
certain species of marine mammals. See Table 5 for the requested
authorized take numbers of marine mammals.
Endangered Species Act
Of the species of marine mammals that may occur in the proposed
survey area, several are listed as endangered under the ESA, including
the humpback, sei, fin, blue, and sperm whales. NSF and ASC did not
request take of endangered Southern right whales due to the low
likelihood of encountering this species during the cruise. Under
section 7 of the ESA, NSF, on behalf of ASC and five other research
institutions, has initiated formal consultation with the NMFS, Office
of Protected Resources, Endangered Species Act Interagency Cooperation
Division, on this proposed seismic survey. NMFS's Office of Protected
Resources, Permits and Conservation Division, has initiated formal
consultation under section 7 of the ESA with NMFS's Office of Protected
Resources, Endangered Species Act Interagency Cooperation Division, to
obtain a Biological Opinion evaluating the effects of issuing the IHA
on threatened and endangered marine mammals and, if appropriate,
authorizing incidental take. NMFS will conclude formal section 7
consultation prior to making a determination on whether or not to issue
the IHA. If the IHA is issued, NSF and ASC, in addition to the
mitigation and monitoring requirements included in the IHA, will be
required to comply with the Terms and Conditions of the Incidental Take
Statement corresponding to NMFS's Biological Opinion issued to both NSF
and ASC, and NMFS's Office of Protected Resources.
National Environmental Policy Act
With NSF and ASC's complete application, NSF and ASC provided NMFS
a ``Draft Initial Environmental Evaluation/Environmental Assessment to
Conduct Marine-Based Studies of the Totten Glacier System and Marine
Record of Cryosphere--Ocean Dynamics,'' (IEE/EA) prepared by AECOM on
behalf of NSF and ASC. The IEE/EA analyzes the direct, indirect, and
cumulative environmental impacts of the proposed specified activities
on marine mammals including those listed as threatened or endangered
under the ESA. Prior to making a final decision on the IHA application,
NMFS will either prepare an independent EA, or, after review and
evaluation of the NSF and ASC IEE/EA for consistency with the
regulations published by the Council of Environmental Quality (CEQ) and
NOAA Administrative Order 216-6, Environmental Review Procedures for
Implementing the National Environmental Policy Act, adopt the NSF and
ASC IEE/EA and make a decision of whether or not to issue a
[[Page 495]]
Finding of No Significant Impact (FONSI).
Proposed Authorization
As a result of these preliminary determinations, NMFS propose to
issue an IHA to NSF and ASC for conducting the low-energy seismic
survey in the tropical western Pacific Ocean, provided the previously
mentioned mitigation, monitoring, and reporting requirements are
incorporated. The proposed IHA language is provided below:
National Science Foundation, Division of Polar Programs, 4201
Wilson Boulevard, Arlington, Virginia 22230 and Antarctic Support
Contract, 7400 South Tucson Way, Centennial, Colorado 80112, is hereby
authorized under section 101(a)(5)(D) of the Marine Mammal Protection
Act (MMPA) (16 U.S.C. 1371(a)(5)(D)), to harass small numbers of marine
mammals incidental to a low-energy marine geophysical (seismic) survey
conducted by the RVIB Nathaniel B. Palmer (Palmer) in the Dumont
d'Urville Sea, Antarctica, January to March 2014:
1. This Authorization is valid from January 29 through April 27,
2014.
2. This Authorization is valid only for the Palmer's activities
associated with low-energy seismic survey operations that shall occur
in the following specified geographic area:
In selected regions of the Dumont d'Urville Sea in the Southern
Ocean off the coast of East Antarctica and focus on the Totten Glacier
and Moscow University Ice Shelf, located on the Sabrina Coast, from
greater than approximately 64[deg] South and between approximately 95
to 135[deg] East, and the Mertz Glacier and Cook Ice Shelf systems
located on the George V and Oates Coast, from greater than
approximately 65[deg] South and between approximately 140 to 165[deg]
East. The study sites are characterized by heavy ice cover, with a
seasonal break-up in the ice that structures biological patterns. The
studies may occur in both areas, or entirely in one or the other,
depending on ice conditions. Water depths in the survey area generally
range from approximately 100 to 1,000 m, and possibly exceeding 1,000 m
in some areas. The low-energy seismic survey will be conducted in
International Waters (i.e., high seas), as specified in NSF and ASC's
Incidental Harassment Authorization application and the associated NSF
and ASC Initial Environmental Evaluation/Environmental Assessment (IEE/
EA).
3. Species Authorized and Level of Takes
(a) The incidental taking of marine mammals, by Level B harassment
only, is limited to the following species in the waters of the Southern
Ocean off the coast of East Antarctica:
(i) Mysticetes--see Table 2 (attached) for authorized species and
take numbers.
(ii) Odontocetes--see Table 2 (attached) for authorized species and
take numbers.
(iii) Pinnipeds--see Table 2 (attached) for authorized species and
take numbers.
(iv) If any marine mammal species are encountered during seismic
activities that are not listed in Table 2 (attached) for authorized
taking and are likely to be exposed to sound pressure levels (SPLs)
greater than or equal to 160 dB re 1 [mu]Pa (rms) for seismic airgun
operations or greater than or equal to 120 dB re 1 [mu]Pa (rms) for
icebreaking activities, then the Holder of this Authorization must
alter speed or course or shut-down the airguns to avoid take.
(b) The taking by injury (Level A harassment), serious injury, or
death of any of the species listed in Condition 3(a) above or the
taking of any kind of any other species of marine mammal is prohibited
and may result in the modification, suspension or revocation of this
Authorization.
4. The methods authorized for taking by Level B harassment are
limited to the following acoustic sources without an amendment to this
Authorization:
(a) A two Generator Injector (GI) airgun array (each with a
discharge volume of 45 cubic inches [in\3\] or 105 in\3\) with a total
volume of 90 in\3\ or 210 in\3\ (or smaller);
(b) A multi-beam echosounder;
(c) A single-beam echosounder;
(d) An acoustic Doppler current profiler;
(e) An acoustic locator;
(f) A sub-bottom profiler; and
(g) Icebreaking.
5. The taking of any marine mammal in a manner prohibited under
this Authorization must be reported immediately to the Office of
Protected Resources, National Marine Fisheries Service (NMFS), at 301-
427-8401.
6. Mitigation and Monitoring Requirements
The Holder of this Authorization is required to implement the
following mitigation and monitoring requirements when conducting the
specified activities to achieve the least practicable adverse impact on
affected marine mammal species or stocks:
(a) Utilize one, NMFS-qualified, vessel-based Protected Species
Observer (PSO) to visually watch for and monitor marine mammals near
the seismic source vessel during daytime airgun operations (from
nautical twilight-dawn to nautical twilight-dusk) and before and during
ramp-ups of airguns day or night. The Palmer's vessel crew shall also
assist in detecting marine mammals, when practicable. PSOs shall have
access to reticle binoculars (7 x 50 Fujinon). PSO shifts shall last no
longer than 4 hours at a time. PSOs shall also make observations during
daytime periods when the seismic airguns are not operating for
comparison of animal abundance and behavior, when feasible.
(b) PSOs shall conduct monitoring while the airgun array and
streamer are being deployed or recovered from the water.
(c) Record the following information when a marine mammal is
sighted:
(i) Species, group size, age/size/sex categories (if determinable),
behavior when first sighted and after initial sighting, heading (if
consistent), bearing and distance from seismic vessel, sighting cue,
apparent reaction to the airguns or vessel (e.g., none, avoidance,
approach, paralleling, etc., and including responses to ramp-up), and
behavioral pace; and
(ii) Time, location, heading, speed, activity of the vessel
(including number of airguns operating and whether in state of ramp-up
or shut-down), Beaufort sea state and wind force, visibility, and sun
glare; and
(iii) The data listed under Condition 6(c)(ii) shall also be
recorded at the start and end of each observation watch and during a
watch whenever there is a change in one or more of the variables.
(d) Visually observe the entire extent of the exclusion zone (180
dB re 1 [mu]Pa [rms] for cetaceans and 190 dB re 1 [mu]Pa [rms] for
pinnipeds; see Table 2 [above] for distances) using NMFS-qualified
PSOs, for at least 30 minutes prior to starting the airgun array (day
or night). If the PSO finds a marine mammal within the exclusion zone,
NSF and ASC must delay the seismic survey until the marine mammal(s)
has left the area. If the PSO sees a marine mammal that surfaces, then
dives below the surface, the PSO shall wait 30 minutes. If the PSO sees
no marine mammals during that time, they should assume that the animal
has moved beyond the exclusion zone. If for any reason the entire
radius cannot be seen for the entire 30 minutes (i.e., rough seas, fog,
darkness), or if marine mammals are near, approaching, or in the
exclusion zone, the airguns may not be ramped-up. If one airgun is
already running at a source level of at
[[Page 496]]
least 180 dB re 1 [mu]Pa (rms), NSF and ASC may start the second airgun
without observing the entire exclusion zone for 30 minutes prior,
provided no marine mammals are known to be near the exclusion zone (in
accordance with Condition 6[f] below).
(e) Establish a 180 dB re 1 [mu]Pa (rms) exclusion zone for
cetaceans and a 190 dB re 1 [mu]Pa (rms) exclusion zone for pinnipeds
before the two GI airgun array (90 or 210 in\3\ total volume) is in
operation. See Table 2 (above) for distances and exclusion zones.
(f) Implement a ``ramp-up'' procedure when starting up at the
beginning of seismic operations or anytime after the entire array has
been shut-down for more than 15 minutes, which means starting with a
single GI airgun and adding a second GI airgun after five minutes.
During ramp-up, the PSOs shall monitor the exclusion zone, and if
marine mammals are sighted, a shut-down shall be implemented as though
the full array (both GI airguns) were operational. Therefore,
initiation of ramp-up procedures from shut-down requires that the PSOs
be able to view the full exclusion zone as described in Condition 6(d)
(above).
(g) Alter speed or course during seismic operations if a marine
mammal, based on its position and relative motion, appears likely to
enter the relevant exclusion zone. If speed or course alteration is not
safe or practicable, or if after alteration the marine mammal still
appears likely to enter the exclusion zone, further mitigation
measures, such as a shut-down, shall be taken.
(h) Shut-down the airgun(s) if a marine mammal is detected within,
approaches, or enters the relevant exclusion zone (as defined in Table
2, above). A shut-down means all operating airguns are shut-down (i.e.,
turned off).
(i) Following a shut-down, the airgun activity shall not resume
until the PSO has visually observed the marine mammal(s) exiting the
exclusion zone and is not likely to return, or has not been seen within
the exclusion zone for 15 minutes for species with shorter dive
durations (small odontocetes and pinnipeds) or 30 minutes for species
with longer dive durations (mysticetes and large odontocetes, including
sperm, killer, and beaked whales).
(j) Following a shut-down and subsequent animal departure, airgun
operations may resume following ramp-up procedures described in
Condition 6(f).
(k) Marine seismic surveys may continue into night and low-light
hours if such segment(s) of the survey is initiated when the entire
relevant exclusion zones are visible and can be effectively monitored.
(l) No initiation of airgun array operations is permitted from a
shut-down position at night or during low-light hours (such as in dense
fog or heavy rain) when the entire relevant exclusion zone cannot be
effectively monitored by the PSO(s) on duty.
7. Reporting Requirements
The Holder of this Authorization is required to:
(a) Submit a draft report on all activities and monitoring results
to the Office of Protected Resources, NMFS, within 90 days of the
completion of the Palmer's Dumont d'Urville Sea off the coast of East
Antarctica cruise. This report must contain and summarize the following
information:
(i) Dates, times, locations, heading, speed, weather, sea
conditions (including Beaufort sea state and wind force), and
associated activities during all seismic operations and marine mammal
sightings;
(ii) Species, number, location, distance from the vessel, and
behavior of any marine mammals, as well as associated seismic activity
(e.g., number of shut-downs), observed throughout all monitoring
activities.
(iii) An estimate of the number (by species) of marine mammals
that: (A) Are known to have been exposed to the seismic activity (based
on visual observation) at received levels greater than or equal to 120
dB re 1 [mu]Pa (rms) (for icebreaking activities), greater than or
equal to 160 dB re 1 [mu]Pa (rms) (for seismic airgun operations), and/
or 180 dB re 1 [mu]Pa (rms) for cetaceans and 190 dB re 1 [mu]Pa (rms)
for pinnipeds with a discussion of any specific behaviors those
individuals exhibited; and (B) may have been exposed (based on modeled
values for the two GI airgun array) to the seismic activity at received
levels greater than or equal to 120 dB re 1 [mu]Pa (rms) (for
icebreaking activities), greater than or equal to 160 dB re 1 [mu]Pa
(rms) (for seismic airgun operations), and/or 180 dB re 1 [mu]Pa (rms)
for cetaceans and 190 dB re 1 [mu]Pa (rms) for pinnipeds with a
discussion of the nature of the probable consequences of that exposure
on the individuals that have been exposed.
(iv) A description of the implementation and effectiveness of the:
(A) Terms and Conditions of the Biological Opinion's Incidental Take
Statement (ITS) (attached); and (B) mitigation measures of the
Incidental Harassment Authorization. For the Biological Opinion, the
report shall confirm the implementation of each Term and Condition, as
well as any conservation recommendations, and describe their
effectiveness, for minimizing the adverse effects of the action on
Endangered Species Act-listed marine mammals.
(b) Submit a final report to the Chief, Permits and Conservation
Division, Office of Protected Resources, NMFS, within 30 days after
receiving comments from NMFS on the draft report. If NMFS decides that
the draft report needs no comments, the draft report shall be
considered to be the final report.
8. In the unanticipated event that the specified activity clearly
causes the take of a marine mammal in a manner prohibited by this
Authorization, such as an injury (Level A harassment), serious injury
or mortality (e.g., ship-strike, gear interaction, and/or
entanglement), NSF and ASC shall immediately cease the specified
activities and immediately report the incident to the Chief of the
Permits and Conservation Division, Office of Protected Resources, NMFS,
at 301-427-8401 and/or by email to Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report must include the following
information:
(a) Time, date, and location (latitude/longitude) of the incident;
the name and type of vessel involved; the vessel's speed during and
leading up to the incident; description of the incident; status of all
sound source use in the 24 hours preceding the incident; water depth;
environmental conditions (e.g., wind speed and direction, Beaufort sea
state, cloud cover, and visibility); description of marine mammal
observations in the 24 hours preceding the incident; species
identification or description of the animal(s) involved; the fate of
the animal(s); and photographs or video footage of the animal (if
equipment is available).
Activities shall not resume until NMFS is able to review the
circumstances of the prohibited take. NMFS shall work with NSF and ASC
to determine what is necessary to minimize the likelihood of further
prohibited take and ensure MMPA compliance. NSF and ASC may not resume
their activities until notified by NMFS via letter, email, or
telephone.
In the event that NSF and ASC discovers an injured or dead marine
mammal, and the lead PSO determines that the cause of the injury or
death is unknown and the death is relatively recent (i.e., in less than
a moderate state of decomposition as described in the next paragraph),
NSF and ASC will immediately report the incident to the Chief of the
Permits and Conservation Division, Office of Protected Resources,
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NMFS, at 301-427-8401, and/or by email to Jolie.Harrison@noaa.gov and
Howard.Goldstein@noaa.gov. The report must include the same information
identified in Condition 8(a) above. Activities may continue while NMFS
reviews the circumstances of the incident. NMFS will work with NSF and
ASC to determine whether modifications in the activities are
appropriate.
In the event that NSF and ASC discovers an injured or dead marine
mammal, and the lead PSO determines that the injury or death is not
associated with or related to the activities authorized in Condition 2
of this Authorization (e.g., previously wounded animal, carcass with
moderate to advanced decomposition, or scavenger damage), NSF and ASC
shall report the incident to the Chief of the Permits and Conservation
Division, Office of Protected Resources, NMFS, at 301-427-8401, and/or
by email to Jolie.Harrison@noaa.gov and Howard.Goldstein@noaa.gov,
within 24 hours of the discovery. NSF and ASC shall provide photographs
or video footage (if available) or other documentation of the stranded
animal sighting to NMFS and the Marine Mammal Stranding Network.
Activities may continue while NMFS reviews the circumstances of the
incident.
9. NSF and ASC is required to comply with the Terms and Conditions
of the ITS corresponding to NMFS's Biological Opinion issued to both
NSF, ASC, and NMFS's Office of Protected Resources (attached).
10. A copy of this Authorization and the ITS must be in the
possession of all contractors and PSOs operating under the authority of
this Incidental Harassment Authorization.
Information Solicited
NMFS requests interested persons to submit comments and information
concerning this proposed project and NMFS's preliminary determination
of issuing an IHA (see ADDRESSES). Concurrent with the publication of
this notice in the Federal Register, NMFS is forwarding copies of this
application to the Marine Mammal Commission and its Committee of
Scientific Advisors.
Dated: December 30, 2013.
P. Michael Payne,
Chief, Permits and Conservation Division, Office of Protected
Resources, National Marine Fisheries Service.
[FR Doc. 2013-31471 Filed 12-31-13; 8:45 am]
BILLING CODE 3510-22-P