Incidental Takes of Marine Mammals During Specified Activities; Low-Energy Marine Seismic Survey in the Northeast Pacific Ocean, July 2009, 24799-24818 [E9-12149]
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Federal Register / Vol. 74, No. 99 / Tuesday, May 26, 2009 / Notices
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24799
Dated: May 19, 2009.
Captain Steven Barnum,
NOAA, Director, Office of Coast Survey,
National Ocean Service, National Oceanic
and Atmospheric Administration.
[FR Doc. E9–12066 Filed 5–22–09; 8:45 am]
BILLING CODE P
DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric
Administration
RIN 0648–XO71
Incidental Takes of Marine Mammals
During Specified Activities; LowEnergy Marine Seismic Survey in the
Northeast Pacific Ocean, July 2009
AGENCY: National Marine Fisheries
Service (NMFS), National Oceanic and
Atmospheric Administration (NOAA),
Commerce.
ACTION: Notice; proposed incidental
take authorization; request for
comments.
SUMMARY: NMFS has received an
application from the Scripps Institution
of Oceanography (SIO), a part of the
University of California San Diego
(UCSD), for an Incidental Harassment
Authorization (IHA) to take small
numbers of marine mammals, by
harassment, incidental to conducting a
marine seismic survey in the Northeast
Pacific Ocean during July 2009.
Pursuant to the Marine Mammal
Protection Act (MMPA), NMFS requests
comments on its proposal to authorize
SIO to incidentally take, by Level B
harassment only, small numbers of
marine mammals during the
aforementioned activity.
DATES: Comments and information must
be received no later than June 25, 2009.
ADDRESSES: Comments on the
application should be addressed to
Michael Payne, Chief, Permits,
Conservation and Education Division,
Office of Protected Resources, National
Marine Fisheries Service, 1315 EastWest Highway, Silver Spring, MD
20910–3225. The mailbox address for
providing email comments is PR1.0648–
XO71@noaa.gov. Comments sent via email, including all attachments, must
not exceed a 10–megabyte file size.
A copy of the application containing
a list of the references used in this
document may be obtained by writing to
the address specified above, telephoning
the contact listed below (see FOR
FURTHER INFORMATION CONTACT), or
visiting the internet at: https://
www.nmfs.noaa.gov/pr/permits/
incidental.htm.
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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 Ken Hollingshead,
Office of Protected Resources, NMFS,
301–713–2289.
SUPPLEMENTARY INFORMATION:
Background
Sections 101(a)(5)(A) and (D) of the
MMPA (16 U.S.C. 1361 et seq.) direct
the Secretary of Commerce to allow,
upon request, the incidental, but not
intentional, taking of marine mammals
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 either regulations are
issued or, if the taking is limited to
harassment, a notice of a proposed
authorization is provided to the public
for review.
Authorization for incidental taking
shall be granted if NMFS finds that the
taking will have a negligible impact on
the species or stock(s), will not have an
unmitigable adverse impact on the
availability of the species or stock(s) for
subsistence uses, and if the permissible
methods of taking and requirements
pertaining to the mitigation, monitoring
and reporting of such takings are set
forth. 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. 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
[ALevel 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
[ALevel B harassment@].
Section 101(a)(5)(D) establishes a 45–
day time limit for NMFS= 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
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20:08 May 22, 2009
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the close of the comment period, NMFS
must either issue or deny issuance of
the authorization.
Summary of Request
On March 9, 2009, NMFS received an
application from SIO for the taking, by
Level B harassment only, of small
numbers of marine mammals incidental
to conducting, under cooperative
agreement with the National Science
Foundation (NSF), a low-energy marine
seismic survey in the Northeast Pacific
Ocean. The funding for the survey is
provided by the NSF. The proposed
survey will occur in an overall area
between approximately 44° and 45° N.
and 124.5° and 126° W. within the
Exclusive Economic Zone (EEZ) of the
U.S.A., and is scheduled to occur from
July 14–20, 2009. The survey will use a
single Generator Injector (GI) airgun
with a discharge volume of 45 in3. Some
minor deviation from these dates is
possible, depending on logistics and
weather.
The proposed survey is virtually
identical to one conducted by SIO in
2007 under an IHA issued in September
2007 (NMFS 2007). The proposed SIO
2009 IHA application contains minor
updates to the project description,
updated marine mammal population
sizes based on the most recent NMFS
annual stock assessment, an assessment
of the relevance of the marine mammal
density and distribution data contained
in the SIO 2007 IHA application based
on cruise reports from the NMFS
SWFSC ORCAWHALE 2008 cruise, and
updated information on effects of
airguns on marine mammals (see
Appendix A of SIO’s application).
Description of the Specified Activity
SIO plans to conduct an ocean bottom
seismograph (OBS) deployment and a
magnetic, bathymetric, and seismic
survey. The planned survey will involve
one source vessel, the R/V Wecoma
(Wecoma), and will occur in the
Northeast Pacific Ocean off the coast of
Oregon.
The purpose of the research program
is to record micro-earthquakes in the
forearc to determine whether seismicity
on the plate boundary is characteristic
of a locked or a freely slipping fault
plane. Several earthquakes large enough
to be recorded on land-based seismic
nets have occurred along this segment
in the past several years. The occurrence
of ‘‘repeating earthquakes’’ (earthquakes
with identical waveforms indicating
repeated rupture of almost the same
fault patch) suggests that this region is
at a boundary between a freely slipping
and a locked portion of the fault. Some
models suggest that the forearc basin
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north of the seismically active zone may
be locked; others suggest that portion of
the fault is slipping freely. OBSs have
been deployed for a year, and a seismic
survey will be used to characterize the
shallow sediment structure around the
instruments. Also, included in the
research is the use of a magnetometer
and sub-bottom profiler.
The source vessel, the Wecoma, will
deploy a single low-energy GI airgun as
an energy source (with a discharge
volume of 45 in3) and a 300 m (984 ft),
16 channel, towed hydrophone
streamer. Sixteen OBSs were deployed
in July and September 2008. They will
continue to acquire data during this
cruise, and will be recovered before
returning to port. The energy to the GI
airgun is compressed air supplied by
compressors onboard the source vessel.
As the GI airgun is towed along the
survey lines, the receiving systems will
receive the returning acoustic signals.
The seismic program will consist of
approximately 21 km (13 mi) of surveys
over each of the 16 OBSs (see Figure 1
of SIO’s application). Water depths at
the seismic survey locations rang from
just less than 100 m (328 ft) to almost
3,000 m (9,842 ft) (see Figure 1 of SIO’s
application). The GI airgun will be
operated on a small grid for
approximately two hours at each of the
16 OBS sites. There will be additional
seismic operations associated with
equipment testing, start-ups, and repeat
coverage of any areas where initial data
quality is substandard.
All planned geophysical data
acquisition activities will be conducted
by SIO with on-board assistance by the
scientists who have proposed the study.
The Chief Scientist is Dr. Anne Trehu of
Oregon State University. The vessel will
be self-contained, and the crew will live
aboard the vessel for the entire cruise.
In addition to the seismic operations
of the single GI airgun, a 3.5 and 12 kHz
sub-bottom profiler will be used
continuously throughout the cruise, and
a magnetometer may be run on the
transit between OBS locations.
Vessel Specifications
The Wecoma has a length of 56.4 m
(185 ft), a beam of 10.1 m (33.1 ft), and
a maximum draft of 5.6 m (18.4 ft). The
ship is powered by a single 3,000–hp
EMD diesel engine driving a single,
controllable-pitch propeller through a
clutch and reduction gear, and an
electric 350–hp azimuthing bow
thruster. An operations speed of 11.1
km/hour (6 knots) will be used during
seismic acquisition. When not towing
seismic survey gear, the Wecoma cruises
at 22.2 km/hour (12 knots) and has a
maximum speed of 26 km/hour (14
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knots). It has a normal operating range
of approximately 13,300 km. The
Wecoma will also serve as the platform
from which vessel-based Marine
Mammal Visual Observers (MMVO) will
watch for animals before and during GI
airgun operations.
Acoustic Source Specifications
Seismic Airguns
During the proposed survey, the
Wecoma will tow a single GI airgun,
with a volume of 45 in3, and a 300 m
long streamer containing hydrophones
along predetermined lines. Seismic
pulses will be emitted at intervals of 10
seconds. At a speed of 6 knots (11.1 km/
hour), the 10 second shot spacing
corresponds to a shot interval of
approximately 31 m (101.7 ft).
The generator chamber of the GI
airgun, the one responsible for
introducing the sound pulse into the
ocean, is 45 in3. The larger (105 in3)
injector chamber injects air into the
previously-generated bubble to maintain
its shape, and does not introduce more
sound into the water. The 45 in3 GI
airgun will be towed 21 m (68.9 ft)
behind the Wecoma at a depth of 4 m
(13.1ft). The sound pressure field of that
GI airgun variation at a tow depth of 2.5
m has been modeled by Lamont-Doherty
Earth Observatory (L-DEO) in relation to
distance and direction for the GI airgun.
As the GI airgun is towed along the
survey line, the towed hydrophone
array in the 300 m streamer receives the
reflected signals and transfers the data
on the on-board processing system.
Given the relatively short streamer
length behind the vessel, the turning
rate of the vessel while the gear is
deployed is much higher than the limit
of five degrees per minute for a seismic
vessel towing a streamer of more typical
length (much greater than 1 km). Thus,
the maneuverability of the vessel is not
limited much during operations.
The root mean square (rms) received
levels that are used as impact criteria for
marine mammals are not directly
comparable to the peak (pk or 0–pk) or
peak-to-peak (pk - pk) values normally
used to characterize source levels of
airgun arrays. The measurement units
used to describe airgun sources, peak or
peak-to-peak decibels, are always higher
than the ‘‘root mean square’’ (rms)
decibels referred to in biological
literature. A measured received level of
160 dB re 1 μPa (rms) in the far field
would typically correspond to a peak
measurement of approximately 170 to
172 dB, and to a peak-to-peak
measurement of approximately 176 to
178 dB, as measured for the same pulse
received at the same location (Greene,
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20:08 May 22, 2009
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1997; McCauley et al., 1998, 2000). The
precise difference between rms and
peak or peak-to-peak values depends on
the frequency content and duration of
the pulse, among other factors.
However, the rms level is always lower
than the peak or peak-to-peak level for
an airgun-type source.
Received sound levels have been
modeled by L-DEO for a number of
airgun configurations, including one 45
in3 GI airgun, in relation to distance
from the airgun(s) (see Figure 2 of SIO’s
application). The model does not allow
for bottom interactions, and is most
directly applicable to deep water. Based
on modeling, estimates of the maximum
distances from the GI airgun where
sound levels of 190, 180, and 160 dB re
1 μPa (rms) are predicted to be received
in deep (≤1,000 m) water are shown in
Table 1 of SIO’s application. Because
the model results are for a 2.5 m tow
depth, the distances in Table 1 slightly
underestimate the distances for the 45
in3 GI airgun towed at 4 m depth.
Sub-bottom Profiler
Along with the GI airgun operations,
one additional acoustical data
acquisition system will be operated
throughout the cruise. The ocean floor
will be mapped with a Knudsen
Engineering Model 320BR 12 kHz and
3.5 kHz sub-bottom profiler (SBP).
Multi-beam sonar will not be used.
The Knudsen Engineering Model
320BR SBP is a dual-frequency
transceiver designed to operate at 3.5
and/or 12 kHz. It is used to provide data
about the sedimentary features that
occur below the sea floor. The energy
from the sub-bottom profiler is directed
downward via a 12 kHz transducer
(EDO 323B) or a 3.5 kHz array of 16 ORE
137D transducers in a 4x4 arrangement.
The maximum power output of the
320BR is 10 kilowatts for the 3.5 kHz
section and 2 kilowatts for the 12 kHz
section.
The pulse length for the 3.5 kHz
section of the 320 BR is 0.8–24 ms,
controlled by the system operator in
regards to water depth and reflectivity
of the bottom sediments, and will
usually be 12 or 24 ms in this survey.
The system produces one sound pulse
and then waits for its return before
transmitting again. Thus, the pulse
interval is directly dependent upon
water depth, and in this survey is 4.5–
8 seconds. Using the Sonar Equations
and assuming 100 percent efficiency in
the system (impractical in real world
applications), the source level for the
320BR is calculated to be 211 dB re 1
Pam. In practical operation, the 3.5 kHz
array is seldom driven at more than 80
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24801
percent of maximum, usually less than
50 percent.
Safety Radii
NMFS has determined that for
acoustic effects, using acoustic
thresholds in combination with
corresponding safety radii is an effective
way to consistently apply measures to
avoid or minimize the impacts of an
action, and to quantitatively estimate
the effects of an action. Thresholds are
used in two ways: (1) to establish a
mitigation shut-down or power-down
zone, i.e., if an animal enters an area
calculated to be ensonified above the
level of an established threshold, a
sound source is powered down or shut
down; and (2) to calculate take, in that
a model may be used to calculate the
area around the sound source that will
be ensonified to that level or above,
then, based on the estimated density of
animals and the distance that the sound
source moves, NMFS can estimate the
number of marine mammals that may be
‘‘taken.’’
As a matter of past practice and based
on the best available information at the
time regarding the effects of marine
sound compiled over the past decade,
NMFS has used conservative numerical
estimates to approximate where Level A
harassment from acoustic sources
begins: 180 dB re 1 μPa (rms) level for
cetaceans and 190 dB re 1 μPa (rms) for
pinnipeds. A review of the available
scientific data using an application of
science-based extrapolation procedures
(Southall et al., 2007) strongly suggests
that Level A harassment (as well as
TTS) from single sound exposure
impulse events may occur at much
higher levels than the levels previously
estimated using very limited data.
However, for purposes of this proposed
action, SIO’s application sets forth, and
NMFS is using, the more conservative
180 and 190 dB re 1 μPa (rms) criteria.
NMFS also considers 160 dB re 1 μPa
(rms) as the criterion for estimating the
onset of Level B harassment from
acoustic sources like impulse sounds
used in the seismic survey.
Emperical data concerning the 180
and 160 dB distances have been
acquired based on measurements during
the acoustic verification study
conducted by L-DEO in the northern
Gulf of Mexico from May 27 to June 3,
2003 (Tolstoy et al., 2004). Although the
results are limited the data showed that
radii around the airguns where the
received level would be 180 dB re 1 μPa
(rms), the safety criterion applicable to
cetaceans (NMFS, 2000), vary with
water depth. Similar depth-related
variation is likely in the 190 dB
distances applicable to pinnipeds.
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Correction factors were developed for
water depths 100–1,000 m and <100 m.
The empirical data indicate that, for
deep water (>1,000 m), the L-DEO
model tends to overestimate the
received sound levels at a given
distance (Tolstoy et al., 2004). However,
to be precautionary pending acquisition
of additional empirical data, it is
proposed that safety radii during GI
airgun operations in deep water will be
values predicted by L-DEO’s model (see
Table 1 below). Therefore, the assumed
180 and 190 dB radii are 23 m (75.5 ft)
and 8 m (26 ft) respectively.
Empirical measurements indicated
that in shallow water (<100 m), the LDEO model under estimates actual
levels. In previous L-DEO projects, the
exclusion zones were typically based on
measured values and ranged from 1.3 to
15x higher than the modeled values
depending on the size of the airgun
array and the sound level measured
(Tolstoy et al., 2004). During the
proposed cruise, similar factors will be
applied to derive appropriate shallow
water radii from the modeled deep
water radii for the GI airgun (see Table
1 below).
Empirical measurements were not
conducted for intermediate depths
(100–1,000 m). On the expectation that
results will be intermediate between
those from shallow and deep water, a
1.5x correction factor is applied to the
estimates provided by the model for
deep water situations. This is the same
factor that was applied to the model
estimates during L-DEO cruises in 2003.
The assumed 180 and 190 dB radii in
intermediate depth water are 35 m (115
ft) and 12 m (39.4 ft), respectively (see
Table 1 below).
TABLE 1. PREDICTED DISTANCES TO WHICH SOUND LEVELS ≥190, 180, AND 160 DB RE 1 μPA MIGHT BE RECEIVED IN
SHALLOW (<100 M; 328 FT), INTERMEDIATE (100–1,000 M; 328–3,280 FT), AND DEEP (>1,000 M; 3,280 FT) WATER
FROM THE SINGLE 45 IN3 GI AIRGUN USED DURING THE SEISMIC SURVEYS IN THE NORTHEASTERN PACIFIC OCEAN
DURING JULY 2009. DISTANCES ARE BASED ON MODEL RESULTS PROVIDED BY L-DEO.
Predicted RMS Distances (m)
Source and Volume
Tow Depth (m)
Water Depth
190 dB
Proposed Dates, Duration, and Region
of Activity
The Wecoma is scheduled to depart
from Newport, Oregon, on July 14, 2009
and to return on July 20, 2009. The GI
airgun will be used for approximately
two hours at each of 16 OBS locations.
The program will consist of
approximately 7 days of seismic
acquisition. The exact dates of the
activities may vary by a few days
because of weather conditions,
repositioning, streamer operations, and
adjustments, GI airgun deployment, or
the need to repeat some lines if data
quality is substandard. The seismic
surveys will take place off the Oregon
coast in the northeastern Pacific Ocean
(see Figure 1 of SIO’s application). The
overall area within which the seismic
surveys will occur is located between
approximately 44° and 45° N and 124.5°
and 126° W (see Figure 1 of SIO’s
application). The surveys will take place
in water depths just less than 100 m and
to almost 3,000 m, entirely within the
Exclusive Economic Zone (EEZ) of the
U.S.A.
Description of Marine Mammals in the
Proposed Activity Area
A total of 32 marine mammal species
may occur or have been documented to
occur in the marine waters off Oregon
and Washington, excluding extralimital
sightings or strandings (Fiscus and
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20:08 May 22, 2009
Jkt 217001
160 dB
Deep (>1,000 m)
8
23
220
12
35
330
Shallow (< 100 m)
4
180 dB
Intermediate (100–
1,000 m)
Single GI airgun 45
in3
95
150
570
Niggol, 1965; Green et al., 1992, 1993;
Barlow, 1997, 2003; Mangels and
Gerrodette, 1994; Von Saunder and
Barlow, 1999; Barlow and Taylor, 2001;
Buchanan et al., 2001; Calambokidis et
al., 2004; Calambokidis and Barlow,
2004). The species include 19
odontocetes (toothed cetaceans, such as
dolphins), 7 mysticetes (baleen whales),
5 pinnipeds, and sea otters. Six of the
species that may occur in the project
area are listed under the Endangered
Species Act (ESA) as Endangered,
including sperm, humpback, sei, fin,
blue, and North Pacific right whales.
Another species, the Steller sea lion, is
listed as Threatened and may occur in
the project area.
The study area is located
approximately 25 to 110 km (15.5 to
68.4 mi) offshore from Oregon over
water depths from just less than 100 m
to almost 3,000 m. Two of the 32
species, gray whales and sea otters, are
not expected in the project area because
their occurrence off Oregon is limited to
very shallow, coastal waters. Three
other species, California sea lions,
Steller sea lions, and harbor seals, are
mainly coastal, and would be rare at
most at the OBS locations. Information
on the habitat, abundance, and
conservation status of the species that
may occur in the study area are given
in Table 2 (below, see Table 2 of SIO’s
application). Vagrant ringed seals,
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hooded seals, and ribbon seals have
been sighted or stranded on the coast of
California (see Mead, 1981; Reeves et
al., 2002) and presumably passed
through Oregon waters. A vagrant
beluga whale was seen off the coast of
Washington (Reeves et al., 2002). Those
seven species are not addressed in detail
in the summaries in SIO’s application.
The six species of marine mammals
expected to be most common in the
deep pelagic or slope waters of the
project area, where most of the survey
sites are located, include the Pacific
white-sided dolphin, northern right
whale dolphin, Risso’s dolphin, short
beaked common dolphin, Dall’s
porpoise, and northern fur seal (Green et
al., 1992, 1993; Buchanan et al., 2001;
Barlow, 2003; Barlow and Forney, 2007;
Carretta et al., 2007). The fin whale,
Dall’s porpoise, and the northern
elephant seal were the species sighted
most often off Oregon and Washington
during the ORCAWALE 2008 surveys
(NMFS, 2008).
Table 2 below outlines the marine
mammal species, their habitat,
abundance, density, and conservation
status in the proposed project area.
Additional information regarding the
distribution of these species expected to
be found in the project area and how the
estimated densities were calculated may
be found in SIO’s application.
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Potential Effects on Marine Mammals
Potential Effects of Airguns
The effects of sounds from airguns
might result in one or more of the
following: tolerance, masking of natural
sounds, behavioral disturbances,
temporary or permanent hearing
impairment, and 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). With the possible
exception of some cases of temporary
threshold shift in harbor seals, it is
unlikely that the project would result in
any cases of temporary or especially
permanent hearing impairment, or any
significant non-auditory physical or
physiological effects.
Tolerance
Numerous studies have shown that
pulsed sounds from airguns are often
readily detectable in the water at
distances of many kilometers. For a brief
summary of the characteristics of airgun
pulses, see Appendix A(3) of SIO’s
application. However, it should be
noted that most of the measurements are
for airguns that would be detectable
considerably farther away than the GI
airgun planned for use in the present
project.
Several studies have shown that
marine mammals at distances more than
a few kilometers from operating seismic
vessels often show no apparent
response-see Appendix A(5) of SIO’s
application. 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 mammal
group. Although various baleen whales,
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toothed whales, and (less frequently)
pinnipeds have been shown to react
behaviorally to airgun pulses under
some conditions, at other times,
mammals of all three types have shown
no overt reactions. In general, pinnipeds
usually seem to be more tolerant of
exposure to airgun pulses than are
cetaceans, with relative responsiveness
of baleen and toothed whales being
variable. Given the relatively small and
low-energy GI airgun source planned for
use in this project, mammals are
expected to be tolerate being closer to
this source than would be the case for
a larger airgun source typical of most
seismic surveys.
Masking
Obscuring of sounds of interest by
interfering sounds, generally at similar
frequencies, is known as masking.
Masking effects of pulsed sounds (even
from large arrays of airguns) on marine
mammal calls and other natural sounds
are expected to be limited, although
there are few specific data of relevance.
Because of the intermittent nature and
low duty cycle of seismic pulses,
animals can emit and receive sounds in
the relatively quiet intervals between
pulses. However in some situations,
multi-path arrivals and reverberation
cause airgun sound to arrive for much
or all of the interval between pulses
(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. The airgun sounds are
pulsed, with quiet periods between the
pulses, and whale calls often can be
heard between the seismic pulses
(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). In the northeast
Pacific Ocean, blue whale calls have
been recorded during a seismic survey
off Oregon (McDonald et al., 1995).
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Among odontocetes, there has been one
report that sperm whales cease calling
when exposed to pulses from a very
distant seismic ship (Bowles et al.,
1994). However, more recent studies
found that sperm whales continued
calling in the presence of seismic pulses
(Madsen et al., 2002; Tyack et al., 2003;
Smultea et al., 2004; Holst et al., 2006;
Jochens et al., 2006, 2008). Given the
small source planned for use during the
proposed survey, there is even less
potential for masking of baleen or sperm
whale calls during the present study
than in most seismic surveys. Masking
effects of seismic pulses are expected to
be negligible in the case of the small
odontocetes given the intermittent
nature of seismic pulses. Dolphins and
porpoises commonly are heard calling
while airguns are operating (Gordon et
al., 2004; Smultea et al., 2004; Holst et
al., 2005a,b; Potter et al., 2007). Also,
the sounds important to small
odontocetes are predominantly at much
higher frequencies than the airgun
sounds, thus further limiting the
potential for masking. In general,
masking effects of seismic pulses are
expected to be minor, given the
normally intermittent nature of seismic
pulses. Masking effects on marine
mammals are discussed further in
Appendix A (4) of SIO’s application.
Disturbance Reactions
Disturbance includes a variety of
effects, including subtle changes in
behavior, more conspicuous changes in
activities, 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. If a marine
mammal responds to an underwater
sound by changing its behavior or
moving a small distance, the response
may or may not rise to the level of
‘‘harassment,’’ or affect the stock or the
species as a whole. However, if a sound
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source displaces marine mammals from
an important feeding or breeding area
for a prolonged period, impacts on
animals or on the stock or species could
potentially be significant (Lusseau and
Bejder, 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 are likely
to be present within a particular
distance of industrial activities, or
exposed to a particular level of
industrial sound. This practice
potentially overestimates the numbers
of marine mammals that are affected in
some biologically-important manner.
The sound exposure thresholds that
are used to estimate how many marine
mammals might be harassed by a
seismic survey are based on behavioral
observations during studies of several
species. However, information is lacking
for many species. Detailed studies have
been done on humpback, gray,
bowhead, and on ringed seals. Less
detailed data are available for some
other species of baleen whales, sperm
whales, small toothed whales, and sea
otters, but for many species there are no
data on responses to marine seismic
surveys. Most of those studies have
concerned reactions to much larger
airgun sources than planned for use in
the proposed project. Thus, effects are
expected to be limited to considerably
smaller distances and shorter periods of
exposure in the present project than in
most of the previous work concerning
marine mammal reactions to airguns.
Baleen Whales – Baleen whales
generally tend to avoid operating
airguns, but avoidance radii are quite
variable. 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, as reviewed in
Appendix A(5) of SIO’s application,
baleen whales exposed to strong noise
pulses from airguns often react by
deviating from their normal migration
route and/or interrupting their feeding
activities and moving away from the
sound source. In the case of the
migrating gray and bowhead whales, the
observed changes in behavior appeared
to be of little or no biological
consequence to the animals. 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 demonstrated
that received levels of pulses in the
160–170 dB re 1 μPa rms range seem to
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cause obvious avoidance behavior in a
substantial fraction of the animals
exposed. In many areas, seismic pulses
from large arrays of airguns diminish to
those levels at distances ranging from
4.5–14.5 km (2.8–9 mi) from the source.
A substantial proportion of the baleen
whales within those distances may
show avoidance or other strong
disturbance reactions to the airgun
array. Subtle behavioral changes
sometimes become evident at somewhat
lower received levels, and studies
summarized in Appendix A(5) of SIO’s
application have shown that some
species of baleen whales, notably
bowhead and humpback whales, at
times show strong avoidance at received
levels lower than 160–170 dB re 1 μPa
(rms). Reaction distances would be
considerably smaller during the
proposed project, for which the 160 dB
radius is predicted to be 220 to 570 m
(722 to 1,870 ft) (see Table 1 above), as
compared with several km when a large
array of airguns is operating.
Responses of humpback whales to
seismic surveys have been studied
during migration, on the summer
feeding grounds, and on Angolan winter
breeding grounds; there has also been
discussion of effects on the Brazilian
wintering grounds. McCauley et al.
(1998, 2000a) studied the responses of
humpback whales off Western Australia
to a full-scale seismic survey with a 16–
airgun, 2,678 in3 array, and to a single
20 in3 airgun with a source level of 227
dB re 1 μPa m peak-to-peak. McCauley
et al. (1998) documented that initial
avoidance reactions began at 5 to 8 km
(3.1 to 5 mi) from the array, and that
those reactions kept most pods
approximately 3 to 4 km (1.9 to 2.5 mi)
from the operating seismic boat.
McCauley et al. (2000) noted localized
displacement during migration of 4 to 5
km (2.5 to 3.1 mi) by traveling pods and
7 to12 km (4.3 to 7.5 mi) by cow-calf
pairs. Avoidance distances with respect
to the single airgun were smaller (2 km
(1.2 mi)) but consistent with the results
from the full array in terms of received
sound levels. The mean received level
for initial avoidance reactions of an
approaching airgun was a sound level of
140 dB re 1 μPa (rms) for humpback
whale pods containing females. The
standoff range, i.e., the closest point of
approach (CPA) of the whales to the
airgun, corresponded to a received level
of 143 dB re 1 μPa (rms). The initial
avoidance response generally occurred
at distances of 5 to 8 km (3.1 to 5 mi)
from the airgun array and 2 km (1.2 mi)
from the single airgun. However, some
individual humpback whales, especially
males, approached within distances of
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100 to 400 m (328 to 1,312 ft), where the
maximum received level was 179 dB re
1 μPa (rms).
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 150–169 dB re 1 μPa
on an approximate rms basis. 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 re 1 μPa on an
approximate rms basis.
Among wintering humpback whales
off Angola (n = 52 useable groups), there
were no significant differences in
encounter rates (sightings/hr) when a 24
airgun array (3,147 in3 or 5,805 in3) was
operating vs. silent (Weir, 2008). There
was also no significant difference in the
mean CPA distance of the humpback
whale sightings when airguns were on
vs. off (3,050 m vs. 2,700 m or 10,007
vs. 8,858 ft, respectively).
It has been 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
results from 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, 2007b:236).
There are no data on reactions of right
whales to seismic surveys, but results
from the closely-related bowhead whale
show that their responsiveness can be
quite variable depending on the activity
(e.g., migrating vs. feeding). Bowhead
whales migrating west across the
Alaskan Beaufort Sea in autumn, in
particular, are unusually responsive,
with substantial avoidance occurring
out to distances of 20–30 km (12.4–18.6
mi) from a medium-sized airgun source
at received sound levels of around 120–
130 dB re 1 μPa (rms) (Miller et al.,
1999; Richardson et al., 1999; see
Appendix B (5) of L-DEO’s application).
However, more recent research on
bowhead whales (Miller et al., 2005a;
Harris et al., 2007) corroborates earlier
evidence that, during the summer
feeding season, bowheads are not as
sensitive to seismic sources.
Nonetheless, subtle but statistically
significant changes in surfacingrespiration-dive cycles were evident
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upon statistical analysis (Richardson et
al., 1986). In summer, bowheads
typically begin to show avoidance
reactions at a received level of about
160–170 dB re 1 μPa (rms) (Richardson
et al., 1986; Ljungblad et al., 1988;
Miller et al., 2005a).
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. Malme et al. (1986,
1988) estimated, based on small sample
sizes, that 50 percent of feeding gray
whales ceased feeding at an average
received pressure level of 173 dB re 1
μPa on an (approximate) rms basis, and
that 10 percent of feeding whales
interrupted feeding at received levels of
163 dB. 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 with observations of Western
Pacific gray whales feeding off Sakhalin
Island, Russia, when a seismic survey
was underway just offshore of their
feeding area (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). Gray whales typically
show no conspicuous responses to
airgun pulses with received levels up to
150 to 160 dB re 1 μPa (rms), but are
increasingly likely to show avoidance as
received levels increase above that
range.
Various species of Balaenoptera (blue,
sei, fin, Bryde’s, and minke whales)
have occasionally been reported in areas
ensonified by airgun pulses (Stone,
2003; MacLean and Haley, 2004; Stone
and Tasker, 2006). Sightings by
observers on seismic vessels off the
United Kingdom from 1997 to 2000
suggest that, at times of good
sightability, sighting rates for mysticetes
(mainly fin and sei whales) were similar
when large arrays of airguns were
shooting and not shooting (Stone, 2003;
Stone and Tasker, 2006). However, these
whales tended to exhibit localized
avoidance, remaining significantly (on
average) from the airgun array during
seismic operations compared with nonseismic periods (Stone and Tasker,
2006). In a study off Nova Scotia,
Moulton and Miller (2005) found little
difference in sighting rates (after
accounting for water depth) and initial
sighting distances of balaenopterid
whales when airguns were operating vs.
silent. However, there were indications
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that these whales were more likely to be
moving away when seen during airgun
operations. Similarly, ship-based
monitoring studies of blue, fin, sei, and
minke whales offshore of
Newfoundland (Orphan Basin and
Laurentian Sub-basin) found no more
than small differences in sighting rates
and swim direction during seismic vs.
non-seismic periods (Moulton et al.,
2005, 2006a,b).
Data on short-term reactions (or lack
of reactions) of cetaceans to impulsive
noises do not necessarily provide
information about long-term effects. It is
not known whether impulsive noises
affect reproductive rate or distribution
and habitat use in subsequent days or
years. However, gray whales 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 (see Appendix A
in Malme et al., 1984; Richardson et al.,
1995; Angliss and Outlaw, 2008). The
Western Pacific gray whale population
did not seem affected by a seismic
survey in its feeding ground during a
prior year (Johnson et al., 2007).
Bowhead whales 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). In
any event, brief exposures to sound
pulses from the proposed airgun source
are highly 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, systematic
studies on sperm whales have been
done (Jochens and Biggs, 2003; Tyack et
al., 2003; Jochens et al., 2006; Miller et
al., 2006), and there is an increasing
amount of information about responses
of various odontocetes to seismic
surveys based on monitoring studies
(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;
Weir, 2008).
Seismic operators and MMOs on
seismic vessels regularly see dolphins
and other small toothed whales near
operating airgun arrays, but in general
there seems to be a tendency for most
delphinids to show some avoidance of
operating seismic vessels (Goold,
1996a,b,c; Calambokidis and Osmek,
1998; Stone, 2003; Moulton and Miller,
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24807
2005; Holst et al., 2006; Stone and
Tasker, 2006; Weir, 2008). 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 airgun arrays are firing
(Moulton and Miller, 2005).
Nonetheless, there have been
indications that small toothed whales
sometimes 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 (Stone and Tasker, 2006; Weir,
2008). In most cases, the avoidance radii
for delphinids appear to be small, on the
order of 1 km (0.62 mi) or less, and
some individuals show no apparent
avoidance. The beluga is a species that
(at least at times) shows long-distance
avoidance of seismic vessels. Aerial
surveys during seismic operations in the
southeastern Beaufort Sea during
summer recorded much lower sighting
rates of beluga whales within 10–20 km
(6.2–12.4 mi) compared with 20–30 km
(mi) from an operating airgun array, and
observers on seismic boats in that area
rarely see belugas (Miller et al., 2005a;
Harris et al., 2007).
Captive bottlenose dolphins and
beluga whales 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;
Finneran and Schlundt, 2004). The
animals tolerated high received levels of
sound (pk-pk level >200 dB re 1 μPa)
before exhibiting aversive behaviors. For
pooled data at 3, 10, and 20 kHz, sound
exposure levels during sessions with 25,
50, and 75 percent altered behavior
were 180, 190, and 199 dB re 1 μPa2,
respectively (Finneran and Schlundt,
2004).
Results for porpoises depend on
species. Dall’s porpoises seem relatively
tolerant of airgun operations (MacLean
and Koski, 2005) and, during a survey
with a large airgun array, tolerated
higher noise levels than did harbor
porpoises and gray whales (Bain and
Williams, 2006). However, Dall’s
porpoises do respond to the approach of
large airgun arrays by moving away
(Calambokidis and Osmek, 1998; Bain
and Williams, 2006). The limited
available data suggest that harbor
porpoises show stronger avoidance
(Stone, 2003; Bain and Williams, 2006;
Stone and Tasker, 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
in general (Richardson et al., 1995;
Southall et al. 2007).
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Most studies of sperm whales exposed
to airgun sounds indicate that this
species shows considerable tolerance of
airgun pulses (Stone, 2003; Moulton et
al., 2005, 2006a; Stone and Tasker,
2006; Weir, 2008). In most cases, the
whales do not show strong avoidance
and continue to call (see Appendix A in
SIO’s application). However, controlled
exposure experiments in the Gulf of
Mexico indicate that foraging effort is
somewhat altered upon exposure to
airgun sounds (Jochens et al., 2006,
2008). In the SWSS study, D-tags
(Johnson and Tyack, 2003) were used to
record the movement and acoustic
exposure of eight foraging sperm whales
before, during, and after controlled
sound exposures of airgun arrays in the
Gulf of Mexico (Jochens et al., 2008).
Whales were exposed to maximum
received sound levels between 111 and
147 dB re 1 μPa (rms) (131 to 164 dB
re 1 μPa pk-pk) at ranges of
approximately 1.4 to 12. 6 km (0.9 to 7.8
mi) from the sound source. Although
the tagged whales showed no horizontal
avoidance, some whales changed
foraging behavior during full array
exposure (Jochens et al., 2008).
There are almost no specific data on
the behavioral reactions of beaked
whales to seismic surveys. However,
northern bottlenose whales (Hyperodon
ampullatus) continued to produce highfrequency clicks when exposed to sound
pulses from distant seismic surveys
(Laurinolli and Cochrane, 2005; Simard
et al., 2005). Most beaked whales tend
to avoid approaching vessels of other
types (Wursig et al., 1998). They may
also dive for an extended period when
approached by a vessel (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 quire long (Baird et
al., 2006; Tyack et al., 2006). In any
event, it is likely that these beaked
whales would normally show strong
avoidance of an approaching seismic
vessel, but this has not been
documented explicitly.
Odontocete reactions to large arrays of
airguns are variable and, at least for
delphinids and Dall’s porpoises, seem to
be confined to a smaller radius than has
been observed for the more responsive
of the mysticetes, belugas, and harbor
porpoises (Appendix A of SIO’s
application).
Additional details on the behavioral
reactions (or the lack thereof) by all
types of marine mammals to seismic
vessels can be found in Appendix A(5)
of SIO’s application.
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Hearing Impairment and Other Physical
Effects
Temporary or permanent hearing
impairment is a possibility when marine
mammals are exposed to very strong
sounds, but there has been no specific
documentation of this for marine
mammals exposed to sequences of
airgun pulses.
NMFS will be developing new noise
exposure criteria for marine mammals
that take account of the now-available
scientific data on temporary threshold
shift (TTS), the expected offset between
the TTS and permanent threshold shift
(PTS) thresholds, differences in the
acoustic frequencies to which different
marine mammal groups are sensitive,
and other relevant factors. Detailed
recommendations for new science-based
noise exposure criteria were published
in late 2007 (Southall et al., 2007).
Several aspects of the planned
monitoring and mitigation measures for
this project (see below) are designed to
detect marine mammals occurring near
the airguns to avoid exposing them to
sound pulses that might, at least in
theory, cause hearing impairment. In
addition, many cetaceans and (to a
limited degree) pinnipeds are likely to
show some avoidance of the area where
received levels of airgun sound are high
enough such that hearing impairment
could potentially occur. In those cases,
the avoidance responses of the animals
themselves will reduce or (most likely)
avoid any possibility of hearing
impairment.
Non-auditory physical effects may
also occur in marine mammals exposed
to strong underwater pulsed sound.
Possible types of non-auditory
physiological effects or injuries that
theoretically might occur in mammals
close to a strong sound source include
stress, neurological effects, bubble
formation, resonance effects, and other
types of organ or tissue damage. It is
possible that some marine mammal
species (i.e., beaked whales) may be
especially susceptible to injury and/or
stranding when exposed to strong
pulsed sounds. However, as discussed
below, there is no definitive evidence
that any of these effects occur even for
marine mammals in close proximity to
large arrays of airguns. It is especially
unlikely that any effects of these types
would occur during the present project
given the brief duration of exposure of
any given mammal and the proposed
monitoring and mitigation measures
(see below). The following subsections
discuss in somewhat more detail the
possibilities of TTS, PTS, and nonauditory physical effects.
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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).
For toothed whales exposed to single
short pulses, the TTS threshold appears
to be, to a first approximation, a
function of the energy content of the
pulse (Finneran et al., 2002, 2005).
Given the available data, the received
level of a single seismic pulse (with no
frequency weighting) might need to be
approximately 186 dB re 1 μPa2.s (i.e.,
186 dB SEL or approximately 221–226
dB pk-pk) in order to produce brief,
mild TTS. Exposure to several strong
seismic pulses that each have received
levels near 190 dB re 1 μPa (rms) (175–
180 dB SEL) might result in cumulative
exposure of approximately 186 dB SEL
and thus slight TTS in a small
odontocete, assuming the TTS threshold
is (to a first approximation) a function
of the total received pulse energy.
Levels ≥ 190 dB 1 μPa (rms) are
expected to be restricted to radii no
more than 95 m (312 ft) from the
Wecoma’s GI airgun. For an odontocete
closer to the surface, the maximum
radius with ≥190 dB 1 μPa (rms) would
be smaller.
The above TTS information for
odontocetes is derived from studies on
the bottlenose dolphin and beluga.
There is not published TTS information
for other species of cetaceans. However,
preliminary evidence from harbor
porpoise exposed to airgun sound
suggests that its TTS threshold may
have been lower (Lucke et al., 2007).
For baleen whales, there are no data,
direct or indirect, on levels or properties
of sound required to induce TTS. The
frequencies to which baleen whales are
most sensitive are lower than those for
odontocetes, 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)
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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. In any
event, no cases of TTS are expected
given three considerations:
(1) Small size of the GI airgun source;
(2) The strong likelihood that baleen
whales would avoid the approaching
airguns (or vessel) before being exposed
to levels high enough for TTS to
possibly occur; and
(3) The mitigation measures that are
planned.
In pinnipeds, TTS thresholds
associated with exposure to brief pulses
(single or multiple) of underwater sound
have not been measured. Initial
evidence from prolonged (non-pulse)
exposures suggested that some
pinnipeds may incur TTS at somewhat
lower received levels than do small
odontocetes exposed for similar
durations (Kastak et al., 1999, 2005;
Ketten et al., 2001; Au et al., 2000). The
TTS threshold for pulsed sounds has
been indirectly estimated as being an
SEL of approximately 171 dB re 1 μPa2.s
(Southall et al., 2007), which would be
equivalent to a single pulse with
received level approximately 181–186 re
1 μPa (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 are likely to be higher
(Kastak et al., 2005).
A marine mammal within a radius of
less than 100 m (328 ft) around a typical
large array of operating airguns might be
exposed to a few seismic pulses with
levels of greater than or equal to 205 dB,
and possibly more pulses if the mammal
moved with the seismic vessel. (As
noted above, most cetacean species tend
to avoid operating airguns, although not
all individuals do so.) In addition,
ramping up airgun arrays, which is
standard operational protocol for large
airgun arrays and proposed for this
action, should allow cetaceans to move
away form the seismic source and avoid
being exposed to the full acoustic
output of the airgun array. Even with a
large airgun array, it is unlikely that the
cetaceans would be exposed to airgun
pulses at a sufficiently high level for a
sufficiently long period to cause more
than mild TTS, given the relative
movement of the vessel and the marine
mammal. The potential for TTS is much
lower in this project. With a large array
of airguns, TTS would be most likely in
any odontocetes that bow-ride or
otherwise linger near the airguns. While
bow-riding, odontocetes would be at or
above the surface, and thus not exposed
to strong pulses given the pressure-
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release effect at the surface. However,
bow-riding animals generally dive
below the surface intermittently. If they
did so while bow-riding near airguns,
they would be exposed to strong sound
pulses, possibly repeatedly. If some
cetaceans did incur TTS through
exposure to airgun sounds, this would
very likely be mild, temporary, and
reversible.
To avoid the potential for injury,
NMFS has determined that cetaceans
and pinnipeds should not be exposed to
pulsed underwater noise at received
levels exceeding, respectively, 180 and
190 dB re 1 μPa (rms). As summarized
above, data that are now available imply
that TTS is unlikely to occur unless
odontocetes (and probably mysticetes as
well) are exposed to airgun pulses
stronger than 180 dB re 1 μPa (rms).
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, while 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
TTS, there has been further speculation
about the possibility that some
individuals occurring very close to
airguns might incur PTS (Richardson et
al., 1995). Single or occasional
occurrences of mild TTS are not
indicative of permanent auditory
damage.
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. PTS might occur at
a received sound level at least several
decibels above that inducing mild TTS
if the animal were exposed to strong
sound pulses with rapid rise time (see
Appendix A(5) of SIO’s application).
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 >6 dB (Southall et al.,
2007). On an SEL basis, Southall et al.
(2007) estimated that received levels
would need to exceed the TTS threshold
by at least 15 dB for there to be risk of
PTS. Thus, for cetaceans they estimate
that the PTS threshold might be an Mweighted SEL (for the sequence of
received pulses) of approximately 198
dB re 1 μPa2μs (15 dB higher than the
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24809
TTS threshold for an impulse).
Additional assumptions had to be made
to derive a corresponding estimate for
pinnipeds, as the only available data on
TTS thresholds in pinnipeds pertain to
non-impulse sound. Southall et al.
(2007) estimate that the PTS threshold
could be a cumulative Mpw-weighted
SEL of approximately 186 dB 1 μPa2.s in
the harbor seal to impulse sound. The
PTS threshold for the California sea lion
and northern elephant seal the PTS
threshold would probably be higher,
given the higher TTS thresholds in
those species.
Southall et al. (2007) also note that,
regardless of the SEL, there is concern
about the possibility of PTS if a cetacean
or pinniped receives one or more pulses
with peak pressure exceeding 230 or
218 dB re 1 μPa (3.2 bar. m, 0–pk),
which would only be found within a
few meters of the largest (600–in3)
airguns in the planned airgun array
(Caldwell and Dragoset, 2000). A peak
pressure of 218 dB re 1 μPa could be
received somewhat farther away; to
estimate that specific distance, one
would need to apply a model that
accurately calculates peak pressures in
the near-field around an array of
airguns.
Given the higher level of sound
necessary to cause PTS as compared
with TTS, it is considerably less likely
that PTS could occur. Baleen whales
generally avoid the immediate area
around operating seismic vessels, as do
some other marine mammals. The
planned monitoring and mitigation
measures, including visual monitoring
and shut downs of the airguns when
mammals are seen about to enter or
within the proposed exclusion zone
(EZ), will further reduce the probability
of exposure of marine mammals to
sounds strong enough to induce PTS,
see the section below on Proposed
Mitigation and Monitoring.
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 effects, and other types of
organ or tissue damage (Cox et al., 2006;
Southall et al., 2007). Studies examining
such effects are limited. However,
resonance (Gentry, 2002) and direct
noise-induced bubble formation (Crum
et al., 2005) are not expected in the case
of an impulsive 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
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specific evidence of this upon exposure
to airgun pulses.
In general, little is known about the
potential for seismic survey sounds to
cause auditory impairment or other
physical effects in marine mammals.
Available data suggest that such effects,
if they occur at all, would presumably
be limited to short distances from the
sound source 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 auditory
impairment or non-auditory physical
effects. Also, the planned mitigation
measures, including shut downs of the
airgun, would reduce any such effects
that might otherwise occur.
Strandings and Mortality
Marine mammals close to underwater
detonations of high explosives can be
killed or severely injured, and their
auditory organs are especially
susceptible to injury (Ketten et al., 1993;
Ketten, 1995). However, explosives are
no longer used for marine seismic
research or commercial seismic surveys,
and have been replaced entirely by
airguns or related non-explosive pulse
generators. Airgun pulses are less
energetic and have slower rise times,
and there is no specific evidence that
they can cause injury, death, or
stranding even in the case of large
airgun arrays. However, the association
of mass strandings of beaked whales
with naval exercises and, in one case, an
L-DEO seismic survey (Malakoff, 2002;
Cox et al., 2006), has raised the
possibility that beaked whales exposed
to strong ‘‘pulsed’’ sounds may be
especially susceptible to injury and/or
behavioral reactions that can lead to
stranding (Hildebrand, 2005; Southall et
al., 2007). Appendix A(5) of SIO’s
application provides additional details.
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 hemorrahage or other
forms of trauma;
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(3) A physiological change such as a
vestibular response leading to a
behavioral change or stress-induced
hemorrahagic 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.
As noted in SIO’s application, some of
these mechanisms are unlikely to apply
in the case of impulse sounds. However,
there are increasing indications that gasbubble disease (analogous to ‘‘the
bends’’), induced in super-saturated
tissue by a behavioral response to
acoustic exposure, could be 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 pulses 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 with most
of the energy below 1 kHz. Typical
military mid-frequency sonars operate at
frequencies of 2–10 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 assume that there
is a direct connection between the
effects of military sonar and seismic
surveys on marine mammals. However,
evidence that sonar pulses can, in
special circumstances, lead (at least
indirectly) to physical damage and
mortality (Balcomb and Claridge, 2001;
NOAA and USN, 2001; Jepson et al.,
2003; Fernandez et al., 2004, 2005a,b;
Hildebrand, 2005; Cox et al., 2006)
suggests that caution is warranted when
dealing with exposure of marine
mammals to any high-intensity pulsed
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) was not well founded based
on available data (IAGC, 2004; IWC,
2006). In September 2002, there was a
stranding of two Cuvier’s beaked whales
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Fmt 4703
Sfmt 4703
(Ziphius cavirostris) in the Gulf of
California, Mexico, when the L-DEO
vessel R/V Maurice Ewing (Ewing) was
operating a 20–gun, 8,490–in3 array in
the general area. The link between the
stranding and the seismic survey 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 when
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, (2) the
proposed monitoring and mitigation
measures, including avoiding submarine
canyons, where deep diving species
may congregate, and (3) differences
between the sound sources operated by
SIO and those involved in the naval
exercises associated with strandings.
Potential Effects of Other Acoustic
Devices
Sub-bottom Profiler Signals
A SBP will be operated from the
source vessel at all times during the
planned study. Sounds from the SBP are
very short pulses, occurring for 12 or 24
ms once every 4.5 to 8 seconds. Most of
the energy in the sound pulses emitted
by the SBP is at mid frequencies,
centered at 3.5 kHz. The beamwidth is
approximately 80° and is directed
downward.
The SBP on the Wecoma has a
maximum source level of 211 dB re 1
μPam. Thus the received level would be
expected to decrease to 180 dB and 160
dB approximately 35 m (115 ft) and 350
m (1,148 ft) below the transducer,
respectively, assuming spherical
spreading. Corresponding distances in
the horizontal plane would be
substantially lower, given the
directionality of this source. Kremser et
al. (2005) noted that the probability of
a cetacean swimming through the area
of exposure when a bottom profiler
emits a pulse is small, and if the animal
was in the area, it would have to pass
the transducer at close range in order to
be subjected to sound levels that could
cause TTS.
Marine mammal communications will
not be masked appreciably by the SBP
signals given their directionality and the
brief period when an individual
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mammal is likely to be within its beam.
Furthermore, in the case of most
odontocetes, the signals do not overlap
with the predominant frequencies in the
calls, which would avoid significant
masking.
Marine mammal behavioral reactions
to other pulsed sound sources are
discussed above, and responses to the
SBP are likely to be similar to those for
other pulsed sources if received at the
same levels. Therefore, behavioral
responses are not expected unless
marine mammals are very close to the
source.
The source levels of the SBP are much
lower than those of the airgun. It is
unlikely that the SBP produces pulse
levels strong enough to cause hearing
impairment or other physical injuries
even in an animal that is (briefly) in a
position near the source. The SBP is
usually operated simultaneously with
other higher-power acoustic sources.
Many marine mammals will move away
in response to the approaching higherpower sources or the vessel itself before
the mammals would be close enough for
there to be any possibility of effects
from the less intense sounds from the
SBP. In the case of mammals that do not
avoid the approaching vessel and its
various sound sources, mitigation
measures that would be applied to
minimize effects of other sources would
further reduce or eliminate any minor
effects of the SBP.
As stated above, NMFS is assuming
that Level A harassment onset
corresponds to 180 and 190 dB re 1 μPa
(rms) for cetaceans and pinnipeds,
respectively. The precautionary nature
of these criteria is discussed in
Appendix A(5) of SIO’s application,
including the fact that the minimum
sound level necessary to cause
permanent hearing impairment is
higher, by a variable and generally
unknown amount, than the level that
induces barely-detectable TTS and the
level associated with the onset of TTS
is often considered to be a level below
which there is no danger of permanent
damage. NMFS also assumes that
cetaceans or pinnipeds exposed to
levels exceeding 160 dB re 1 μPa (rms)
may experience Level B harassment.
Possible Effects of Acoustic Release
Signals
The acoustic release transponder used
to communicate with the OBSs uses
frequencies of 9–13 kHz. Once the OBS
is ready to be retrieved, an acoustic
release transponder interrogates the
OBS at a frequency of 9–11 kHz, and a
response is received at a frequency of 9–
13 kHz. The burn wire release is then
activated, and the instrument is released
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from the anchor to float to the surface.
These signals will be used very
intermittently. It is unlikely that the
acoustic release signals would have
effects on marine mammals through
masking, disturbance, or hearing
impairment. Any effects likely would be
de minimus given the brief exposure at
low levels.
Estimated Take by Incidental
Harassment
All anticipated takes would be ‘‘takes
by harassment,’’ involving temporary
changes in behavior. The proposed
monitoring and mitigation measures are
expected to minimize the possibility of
injurious takes. (However, as noted
earlier, there is no specific information
demonstrating that injurious ‘‘takes’’
would occur even in the absence of the
planned monitoring and mitigation
measures.) The sections below describe
methods to estimate ‘‘take by
harassment’’, and present estimates of
the numbers of marine mammals that
might be affected during the proposed
seismic program. The estimates of ‘‘take
by harassment’’ are based on (1) data
concerning marine mammal densities
(numbers per unit area) obtained during
surveys off Oregon and Washington
during 1996, 2001, and 2005
(cetaceans), or 1989 to 1990 (pinnipeds)
by NMFS Southwest Fisheries Science
Center (SWFSC), and (2) estimates of the
size of the 160 dB isolpeths where takes
could potentially occur from the
proposed seismic survey off the coast of
Oregon in the northeastern Pacific
Ocean.
Extensive systematic aircraft and
ship-based surveys have been
conducted for marine mammals offshore
of Oregon and Washington (Bonnell et
al., 1992; Green et al., 1992, 1993;
Barlow 1997, 2003; Barlow and Taylor,
2001; Calambokidis and Barlow, 2004;
Barlow and Forney in prep.). The most
comprehensive and recent density data
available for cetacean species in slope
and offshore waters of Oregon are from
the 1996, 2001, and 2005 NMFS SWFSC
‘‘ORCAWALE’’ or ‘‘CSCAPE’’ ship
surveys as synthesized by Barlow and
Forney (2007). The surveys were
conducted up to approximately 550 km
(342 mi) offshore from June or July to
November or December. Systematic,
offshore, at-sea survey data for
pinnipeds are more limited. The most
comprehensive such studies are
reported by Bonnell et al. (1992) based
on systematic aerial surveys conducted
in 1989–1990.
Oceanographic conditions, including
occasional El Nino and La Nina events,
influence the distribution and numbers
of marine mammals present in the
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Sfmt 4703
24811
Northeast Pacific Ocean, including
Oregon, resulting in considerable yearto-year variation in the distribution and
abundance of many marine mammal
species (Forney and Barlow, 1998;
Buchanan et al., 2001; Escorza-Trevino,
2002; Ferrero et al., 2002; Philbrick et
al., 2003). Thus, for some species the
densities derived from recent surveys
may not be representative of the
densities that will be encountered
during the proposed seismic survey. For
this IHA application, cruise reports from
the ORCAWALE 2008 surveys (NMFS,
2008) were inspected to assess whether
there were any observable changes from
the previous surveys of the same area.
Table 3 of SIO’s application gives the
average and maximum densities for
each species of cetacean reported off
Oregon and Washington, corrected for
effort, based on the densities reported
for the 1996, 2001, and 2005 surveys
(Barlow and Forney, 2007). The
densities from those studies had been
corrected, by the original authors, for
both detectability bias and availability
bias. Detectability bias is associated
with diminishing sightability with
increasing lateral distance from the
trackline. Availability bias refers to the
fact that there is <100 percent
probability of sighting an animals that is
present along the survey trackline.
Table 3 of SIO’s application also
includes mean density information for
three of the five pinnipeds species that
occur off Oregon and Washington and
mean and maximum densities for one of
those species, from Bonnell et al. (1992).
Densities were not calculated for the
other two species because of the small
number of sightings on systematic
transect surveys. One of those, the
northern elephant seal, was the
dominant seal sighted during the
ORCAWALE 2008 surveys (29 of 33
pinnipeds sighted off Oregon and
Washington), so it was included at a
density set at twice that of the northern
fur seal, the other species sighted during
the ORCAWALE 2008 surveys.
It should be noted that the following
estimates of ‘‘takes by harassment’’
assume that the surveys will be
undertaken and completed; in fact, the
planned number of line kms has been
increased by 25 percent to accommodate
lines that may need to be repeated,
equipment testing, etc. As is typical on
offshore ship surveys, inclement
weather, and equipment malfunctions
are likely to cause delays and may limit
the number of useful line kms of seismic
operations that can be undertaken.
Furthermore, any marine mammal
sightings within or near the designated
safety zones will result in the shutdown of seismic operations as a
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mitigation measure. Thus, the following
estimates of the numbers of marine
mammals potentially exposed to 160 dB
are precautionary, and probably
overestimate the actual numbers of
marine mammals that might be
involved. These estimates assume that
there will be no weather, equipment, or
mitigation delays, which is highly
unlikely.
There is some uncertainty about the
representativness of the data and the
assumption used in the calculations.
However, the approach used is believed
to be the best available approach. Also,
to provide some allowance for these
uncertainties ‘‘maximum estimates’’ as
well as ‘‘best estimates’’ of the numbers
potentially affected have been derived.
Best and maximum estimates are based
on the average and maximum estimates
of densities reported primarily by
Barlow and Forney (2007) and Bonnell
et al. (1992) described above. The
estimated numbers of potential
individuals exposed are presented
below based on the 160 dB re 1 μPa
(rms) Level B harassment criterion for
all cetaceans and pinnipeds. It is
assumed that a marine mammal exposed
to airgun sounds this strong might
change their behavior sufficiently to be
considered ‘‘taken by harassment.’’
The number of different individuals
that may be exposed to GI airgun sounds
with received levels ≥160 dB re 1 μPa
(rms) on one or more occasions was
estimated by considering the total
marine area that would be within the
160 dB radius around the operating
airgun array on at least one occasion.
The proposed seismic lines do not run
parallel to each other in close proximity,
which minimizes the number of times
an individual mammal may be exposed
during the survey. The best estimates in
this section are based on the averages of
the densities from the 1996, 2001, and
2005 NMFS surveys, and maximum
estimates are based on the highest of the
three densities. Table 4 of SIO’s
application and Table 2 of this Federal
Register notice show the best and
maximum estimates of the number of
marine mammals that could potentially
be affected during the seismic survey.
The number of different individuals
potentially exposed to received levels
≥160 dB re 1 μPa (rms) was calculated
by multiplying:
• The expected species density, either
‘‘mean’’ (i.e., best estimate) or
‘‘maximum,’’ times; and
• The area anticipated to be
ensonified to that level during GI airgun
operations.
The area expected to be ensonified
was determined by entering the planned
survey lines into a MapInfo Geographic
Information System (GIS), using the GIS
to identify the relevant areas by
‘‘drawing’’ the applicable 160 dB buffer
around each seismic line (depending on
water and tow depth) and then
calculating the total area within the
buffers. Areas where overlap occurred
(because of intersecting lines) were
included only once to determine the
area expected to be ensonified. In the
proposed survey, there is minimal
overlap (5 percent for 160 dB), so
virtually no marine mammal would be
ensonified above those thresholds more
than once.
Applying the approach described
above, approximately 208 km2 (80.3
mi2) would be within the 160 dB
isopleth on one or more occasions
during the surveys at all 16 OBS
locations. For inshore OBS locations,
approximately 60 km2 (23 mi2) would
be within the 160 dB isopleths; that area
was used for calculations for the
pinniped species that could occur only
at those locations. This approach does
not allow for turnover in the mammal
populations in the study area during the
course of the surveys. That might
underestimate actual numbers of
individuals exposed, although the
conservative distances used to calculate
the area may offset this. In addition, the
approach assumes that no cetaceans will
move away or toward the trackline as
the Wecoma approaches, in response to
increasing sound levels prior to the time
the levels reach 160 dB. Another way of
interpreting the estimates that follow in
Table 3 (below) is that they represent
the number of individuals that are
expected (in the absence of a seismic
program) to occur in the waters that will
be exposed to ≥160 dB re 1 μPa (rms).
TABLE 3. THE ESTIMATES OF THE POSSIBLE NUMBERS OF MARINE MAMMALS EXPOSED TO SOUND LEVELS GREATER THAN
OR EQUAL TO 160 DB DURING SIO’S PROPOSED SEISMIC SURVEY OFF OREGON IN JULY 2009. THE PROPOSED SOUND
SOURCE IS A SINGLE GI AIRGUN. RECEIVED LEVELS ARE EXPRESSED IN DB RE 1 μPA (RMS) (AVERAGED OVER PULSE
DURATION), CONSISTENT WITH NMFS’ PRACTICE. NOT ALL MARINE MAMMALS WILL CHANGE THEIR BEHAVIOR WHEN EXPOSED TO THESE SOUND LEVELS, BUT SOME MAY ALTER THEIR BEHAVIOR WHEN LEVELS ARE LOWER (SEE TEXT). SEE
TABLES 2–4 IN SIO’S APPLICATION FOR FURTHER DETAIL.
# of Individuals Exposed
(best)1
# of Individuals Exposed
(max)1
Approx. % Regional
Population (best)2
Eastern Pacific gray whale
(Eschrichtius robustus)
0
0
0
North Pacific right whale
(Eubalaena japonica)
0
0
0
Humpback whale
(Megaptera novaeangliae)
0
2
0
Minke whale(Balaenoptera acutorostrata)
0
0
0
Sei whale(Balaenoptera borealis)
0
0
0
Fin whale
(Balaenoptera physalus)
0
1
0
Blue whale
(Balaenoptera musculus)
0
1
0
Species
Mysticetes
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TABLE 3. THE ESTIMATES OF THE POSSIBLE NUMBERS OF MARINE MAMMALS EXPOSED TO SOUND LEVELS GREATER THAN
OR EQUAL TO 160 DB DURING SIO’S PROPOSED SEISMIC SURVEY OFF OREGON IN JULY 2009. THE PROPOSED SOUND
SOURCE IS A SINGLE GI AIRGUN. RECEIVED LEVELS ARE EXPRESSED IN DB RE 1 μPA (RMS) (AVERAGED OVER PULSE
DURATION), CONSISTENT WITH NMFS’ PRACTICE. NOT ALL MARINE MAMMALS WILL CHANGE THEIR BEHAVIOR WHEN EXPOSED TO THESE SOUND LEVELS, BUT SOME MAY ALTER THEIR BEHAVIOR WHEN LEVELS ARE LOWER (SEE TEXT). SEE
TABLES 2–4 IN SIO’S APPLICATION FOR FURTHER DETAIL.—Continued
# of Individuals Exposed
(best)1
# of Individuals Exposed
(max)1
Approx. % Regional
Population (best)2
Sperm whale
(Physeter macrocephalus)
0
8
0
Pygmy sperm whale
(Kogia breviceps)
0
1
N.A.
Dwarf sperm whale
(Kogia sima)
0
0
0
Cuvier’s beaked whale
(Ziphius cavirostris)
0
0
0
Baird’s beaked whale
(Berardius bairdii)
0
1
0
Blainville’s beaked whale
(Mesoplodon densirostris)
0
0
0
Hubb’s beaked whale(Mesoplodon carlhubbsi)
0
0
0
Stejneger’s beaked whale
(Mesoplodon stejnegeri)
0
0
0
Mesoplodon sp.
(unidentified)
0
1
0
Offshore bottlenose dolphin
(Tursiops truncatus)
0
0
0
Striped dolphin
(Stenella coeruleoalba)
0
0
0
Short-beaked common dolphin
(Delphinus delphis)
4
9
<0.01
Pacific white-sided dolphin
Lagenorhynchus obliquidens)
6
9
0.02
Northern right-whale dolphin
(Lissodelphis borealis)
5
7
0.02
Risso’s dolphin
(Grampus griseus)
3
4
0.03
False killer whale
(Pseudorca crassidens)
0
0
N.A.
Killer whale
(Orcinus orca)
0
1
0
Short-finned pilot whale
(Globicephala macrorhynchus)
Harbor porpoise
(Phocoena phocoena)
0
0
0
0
0
0
Dall’s porpoise
(Phocoenoides dalli)
39
65
0.1
3
26
<0.01
Species
Odontocetes
Pinnipeds
Northern fur seal
(Callorhinus ursinus)
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TABLE 3. THE ESTIMATES OF THE POSSIBLE NUMBERS OF MARINE MAMMALS EXPOSED TO SOUND LEVELS GREATER THAN
OR EQUAL TO 160 DB DURING SIO’S PROPOSED SEISMIC SURVEY OFF OREGON IN JULY 2009. THE PROPOSED SOUND
SOURCE IS A SINGLE GI AIRGUN. RECEIVED LEVELS ARE EXPRESSED IN DB RE 1 μPA (RMS) (AVERAGED OVER PULSE
DURATION), CONSISTENT WITH NMFS’ PRACTICE. NOT ALL MARINE MAMMALS WILL CHANGE THEIR BEHAVIOR WHEN EXPOSED TO THESE SOUND LEVELS, BUT SOME MAY ALTER THEIR BEHAVIOR WHEN LEVELS ARE LOWER (SEE TEXT). SEE
TABLES 2–4 IN SIO’S APPLICATION FOR FURTHER DETAIL.—Continued
# of Individuals Exposed
(best)1
# of Individuals Exposed
(max)1
Approx. % Regional
Population (best)2
N.A.
N.A.
N.A.
Steller sea lion
(Eumetopias jubatus)
1
N.A.
<0.01
Harbor seal
(Phoca vitulina richardsi)
1
N.A.
<0.01
Northern elephant seal
(Mirounga angustirostris)
5
52
<0.01
Species
California sea lion
(Zalophus californianus)
N.A.—Data not available or species status was not assessed
1 Best estimate and maximum estimate density are from Table 3 of SIO’s application.
2 Regional population size estimates are from Table 2 (above).
Table 4 of SIO’s application shows the
best and maximum estimates of the
number of exposures and the number of
individual marine mammals that
potentially could be exposed to greater
than or equal to 160 dB re 1 μPa (rms)
during the different legs of the seismic
survey if no animals move away from
the survey vessel.
The ‘‘best estimate’’ of the number of
individual marine mammals that could
be exposed to seismic sounds with
received levels greater than or equal to
160 dB re 1 μPa (rms) (but below Level
A harassment thresholds) during the
survey is shown in Table 4 of SIO’s
application and Table 3 (shown above).
The maximum estimates have been
requested by SIO. The ‘‘best estimate’’
total includes 0 baleen whale
individuals. These estimates were
derived from the best density estimates
calculated for these species in the area
(see Table 4 of SIO’s application). In
addition, 0 sperm whales (0 percent of
the regional population) as well as 0
beaked whales (0 percent of the regional
population). Based on the best
estimates, most (85.1 percent) of the
marine mammals potentially exposed
are dolphins and porpoises; shortbeaked common, Pacific white-sided,
Northern right-whale, Risso’s dolphins
and Dall’s porpoises are estimated to be
the most common species in the area,
with best estimates of 4 (<0.01 percent
of the regional population), 6 (0.02
percent), 5 (0.02 percent), 3 (0.03
percent), and 39 (0.01 percent) exposed
to greater or equal to 160 dB re μPa
(rms) respectively. The remainder of the
marine mammals that may be
potentially exposed are pinnipeds;
Northern fur, harbor, and Northern
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elephant seals, and Steller sea lions are
estimated to be the most common
species in the area, with best estimates
of 3 (<0.01 percent), 1 (<0.01 percent),
5 (<0.01 percent), and 1 (<0.01 percent)
exposed to greater or equal to 160 dB re
μPa (rms) respectively. Haul-outs of
California sea lions and harbor seals are
known to be located in the Newport,
Oregon area. All of these numbers are
considered small relative to the
population sizes of the affected species
or stocks.
Potential Effects on Marine Mammal
Habitat
The proposed SIO seismic survey will
not result in any permanent impact on
habitats used by marine mammals, or to
the food sources they use. The main
impact issue associated with the
proposed activity will be temporarily
elevated noise levels and the associated
direct effects on marine mammals, as
described above. The following sections
briefly review effects of airguns on fish
and invertebrates, and more details are
included in SIO’s application and EA.
Potential Effects on Fish and
Invertebrates
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 populations is very limited (see
Appendix B of SIO’s application). There
are three types of potential effects on
fish and invertebrates from exposure to
seismic surveys: (1) pathological, (2)
physiological, and (3) behavioral.
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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 potentially could
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. 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 aspect of potential
impacts relates to how exposure to
seismic survey sound affects marine fish
populations and their viability,
including their availability to fisheries.
The following sections provide a
general synopsis of 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
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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 then 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 (see Appendix B of
SIO’s application). For a given sound to
result in hearing loss, the sound must
exceed, by some specific 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 is unknown;
however, it likely depends 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 we know,
there are only two valid papers with
proper experimental methods, controls,
and careful pathological investigation
implicating sounds produced by actual
seismic survey airguns with 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
(Coreogonus nasus) that received a
sound exposure level of 177 dB re 1
μPa2.s showed no hearing loss. 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
airgun arrays [less than approximately
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
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(approximately 9 m in the former case
and less than 2 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 and invertebrates 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; Hassel et
al., 2003; Popper et al., 2005).
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. 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;
McCauley et al., 2000a, 2000b). 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
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24815
stimulus (see Appendix B of SIO’s
application).
Summary of Physical (Pathological
and Physiological) Effects – As
indicated in the preceding general
discussion, there is a relative lack of
knowledge about the potential physical
(pathological and physiological) effects
of seismic energy on marine fish and
invertebrates. Available data suggest
that there may be physical impacts on
egg, larval, juvenile, and adult stages at
very close range. Considering typical
source levels associated with
commercial seismic arrays, close
proximity to the source would result in
exposure to very high energy levels.
Whereas egg and larval stages are not
able to escape such exposures, juveniles
and adults most likely would avoid it.
In the case of eggs and larvae, it is likely
that the numbers adversely affected by
such exposure would not be that
different from those succumbing to
natural mortality. Limited data
regarding physiological impacts on fish
and invertebrates indicate that these
impacts are short term and are most
apparent after exposure at close range.
The proposed seismic program for
2009 is predicted to have negligible to
low physical effects on the various stags
of fish and invertebrates for its relatively
short duration (approximately 7 days)
and unique survey lines extent.
Therefore, physical effects of the
proposed program on fish and
invertebrates would not be significant.
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 (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.
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
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impinging sound field and not to the
pressure component (Popper et al.,
2001; see Appendix C of SIO’s
application).
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.
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 C of SIO’s
application.
Pathological Effects – In water, lethal
and sub-lethal injury to organisms
exposed to seismic survey sound could
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 single GI gun 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; 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
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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 there is no
evidence to support such claims.
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. Any primary and
secondary stress responses (i.e., changes
in haemolymph levels of enzymes,
proteins, etc.) of crustaceans after
exposure to seismic survey sounds
appear to be temporary (hours to days)
in studies done to date (J. Payne, DFO,
pers. comm.). 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. Change in behavior could
potentially affect such aspects as
reproductive success, distribution,
susceptibility to predation, and
catchability by fisheries. Studies
investigating the possible behavioral
effect of exposure to seismic survey
sound on crustaceans and cephalopods
have been conducted on both uncaged
and caged animals. In some cases,
invertebrates exhibiting 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
reduced catch rates of shrimp shortly
after exposure to seismic surveys;
however, other studies have not
observed any significant changes in
shrimp and catch rate (AndriguiettoFilho et al., 2005). 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).
Because of the reasons noted above
and the nature of the proposed
activities, the proposed operations are
not expected to cause significant
impacts on habitats that could cause
significant or long-term consequences
for individual marine mammals or their
populations or stocks. Similarly, any
effects to food sources are expected to
be negligible.
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Subsistence Activities
There is no subsistence hunting for
marine mammals in the waters off of the
coast of Oregon that implicates MMPA
Section 101(a)(5)(D).
Proposed Mitigation and Monitoring
Mitigation and monitoring measures
proposed to be implemented for the
proposed seismic survey have been
developed and refined during previous
SIO and NSF-funded seismic studies
and associated environmental
assessments (EAs), IHA applications,
and IHAs. The mitigation and
monitoring measures described herein
represent a combination of procedures
required by past IHAs for other similar
projects and on recommended best
practices in Richardson et al. (1995),
Pierson et al. (1998), and Weir and
Dolman (2007). The measures are
described in detail below.
Mitigation measures that will be
adopted during the proposed survey
include:
(1) Speed or course alteration,
provided that doing so will not
compromise operational safety
requirements;
(2) GI airgun shut-down procedures;
and
(3) Special procedures for situations
or species of particular concern, e.g.,
emergency shut-down procedures if a
North Pacific right whale and
minimization of approaches to slopes, if
possible, to avoid beaked whale habitat.
Two other common mitigation
measures, airgun array power-down and
airgun array ramp-up, are not possible
because only one, low-volume GI airgun
will be used for the surveys. The
thresholds for estimating Level A
harassment take are also used in
connection with proposed mitigation.
Vessel-based Visual Monitoring
Marine Mammal Visual Observers
(MMVOs) will be based aboard the
seismic source vessel and will watch for
marine mammals near the vessel during
daytime airgun operations and during
start-ups of airguns at night. MMVOs
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 shutdown of the airguns. When feasible
MMVOs will also make observations
during daytime periods when the
seismic system is not operating for
comparison of sighting rates and animal
behavior with vs. without airgun
operations. Based on MMVO
observations, the GI airgun will be shutdown (see below) when marine
mammals are detected within or about
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to enter a designated EZ that
corresponds to the 180 or 190 dB re 1
μPa (rms) isopleths, depending on
whether the animal is a cetacean or
pinniped . The MMVOs will continue to
maintain watch to determine when the
animal(s) are outside the EZ, and airgun
operations will not resume until the
animal has left that EZ. The predicted
distances for the 180, and 190 dB EZs
are listed according to the water depth
in Table 1 above.
During seismic operations off of the
coast of Oregon, at least two MMVOs
will be based aboard the Wecoma.
MMVOs will be appointed by SIO with
NMFS concurrence. At least one MMVO
will monitor the EZ for marine
mammals during ongoing daytime GI
airgun operations and nighttime
startups of the airguns. MMVO(s) will
be on duty in shifts no longer than 4
hours duration. The vessel crew will
also be instructed to assist in detecting
marine mammals and implementing
mitigation measures (if practical). Before
the start of the seismic survey the crew
will be given additional instruction
regarding how to do so.
The Wecoma is a suitable platform for
marine mammal observations.
Observing stations will be on the bridge
wings, with observers’ eyes
approximately 6.5 m (21.3 ft) above the
waterline and a 180 degree view
outboard from either side, on the
whaleback deck in front of the bridge,
with observers eyes approximately 7 m
(23 ft) above the waterline and
approximately 200 degrees view
forward, and on the aft control station,
with observer’s eyes approximately 5.5
m (18 ft) above the waterline and a
approximately 180 degree view aft that
includes the 40 m (131 ft) (180 dB)
radius area around the GI airgun. The
eyes of the bridge watch will be at a
height of approximately 6.5 m; MMOs
will repair to the enclosed bridge during
any inclement weather.
During the daytime, the MMVO(s)
will scan the area around the vessel
systematically with reticle binoculars
(e.g., 7x50), Big-eye binoculars (25x150),
optical range finders, and with the
naked eye. During darkness, night
vision devices will be available, when
required. The MMVOs will be in
wireless 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 GI airgun shut
down.
Speed or Course Alteration – If a
marine mammal is detected outside the
EZ but is likely to enter based on its
position and the relative movement of
the vessel and animal, then if safety and
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scientific objectives allow, the vessel
speed and/or course may be adjusted to
minimize the likelihood of the animal
entering the EZ. Typically, during
seismic operations, major course and
speed adjustments are often impractical
when towing long seismic streamers and
large source arrays, but are possible in
this case because only one GI airgun and
a short streamer will be used.
Shut-down Procedures – The
operating airguns(s) will be shut-down
if a marine mammal is detected within
or approaching the EZ for the single GI
airgun source. Following a shut-down,
GI airgun activity will not resume until
the marine mammal is outside the EZ
for the full array. The animal will be
considered to have cleared the EZ if it:
• Is visually observed to have left the
EZ;
• Has not been seen within the EZ for
15 min in the case of species with
shorter dive durations - small
odontocetes and pinnipeds; and
• Has not been seen within the EZ for
30 min in the case of species with
longer dive durations - mysticetes and
large odontocetes, including sperm,
pygmy sperm, dwarf sperm, killer, and
beaked whales.
Procedures for Situations or Species
of Particular Concern – Special
mitigation procedures will be used for
these species of particular concern as
follows:
(1) The GI airgun will be shut-down
if a North Pacific right whale is sighted
at any distance from the vessel;
(2) To avoid beaked whale habitat,
approach to slopes will be minimized,
if possible, during the proposed survey.
Avoidance of airgun operations over or
near submarine canyons has become a
standard mitigation measure, but there
are none within or near the study area.
Four of the 16 OBS locations are on the
continental slope, but the GI airgun is
low volume and it will operate only for
a short time (approximately 2 hours at
each location).
SIO and NSF will coordinate the
planned marine mammal monitoring
program associated with the seismic
survey off the coast of Oregon with
applicable U.S. agencies (e.g., NMFS),
and will comply with their
requirements.
Proposed Reporting
MMVO Data and Documentation
MMVOs 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
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24817
harassment (as defined in the MMPA).
They will also provide information
needed to order a shutdown of the
seismic source when a marine mammal
or sea turtles is within or near the EZ.
When a sighting is made, the
following information about the sighting
will be recorded:
(1) Species, group size, and 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,
visibility, cloud cover, and sun glare.
The data listed (time, location, etc.)
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 seismic source
shut-down, will be recorded in a
standardized format. Data accuracy will
be verified by the MMVOs at sea, and
preliminary reports will be prepared
during the field program and summaries
forwarded to the operating institution’s
shore facility and to NSF weekly or
more frequently. MMVO observations
will provide the following information:
(1) The basis for decisions about
shutting down airgun arrays.
(2) Information needed to estimate the
number of marine mammals potentially
’taken by harassment.’ These data will
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) Data on the behavior and
movement patterns of marine mammals
seen at times with and without seismic
activity.
A report will be submitted 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 will be submitted
to NMFS, providing 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 (dates, times,
locations, activities, associated seismic
survey activities). The report will also
include estimates of the amount and
nature of potential ‘‘take’’ of marine
mammals by harassment or in other
ways.
E:\FR\FM\26MYN1.SGM
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Federal Register / Vol. 74, No. 99 / Tuesday, May 26, 2009 / Notices
All injured or dead marine mammals
(regardless of cause) will be reported to
NMFS as soon as practicable. The report
should include species or description of
animal, condition of animal, location,
time first found, observed behaviors (if
alive) and photo or video, if available.
Endangered Species Act (ESA)
Under Section 7 of the ESA, NSF has
begun consultation with the NMFS,
Office of Protected Resources,
Endangered Species Division on this
proposed seismic survey. NMFS will
also consult on the issuance of an IHA
under section 101(a)(5)(D) of the MMPA
for this activity. Consultation will be
concluded prior to a determination on
the issuance of the IHA.
National Environmental Policy Act
(NEPA)
NSF prepared a draft Environmental
Assessment titled ‘‘Marine Seismic
Survey in the Northeast Pacific, July
2009.’’ NSF’s draft EA incorporates an
‘‘Environmental Assessment (EA) of a
Planned Low-Energy Marine Seismic
Survey by the Scripps Institution of
Oceanography in the Northeast Pacific
Ocean, July 2009’’ prepared by LGL
Limited, Environmental Research
Associates, on behalf of NSF and SIO.
NMFS will either adopt NSF’s EA or
conduct a separate NEPA analysis, as
necessary, prior to making a
determination on the issuance of the
IHA.
Preliminary Determinations
NMFS has preliminarily determined
that the impact of conducting the lowenergy marine seismic survey in the
Northeast Pacific Ocean may result, at
worst, in a temporary modification in
behavior (Level B harassment) of small
numbers of marine mammals. Further,
this activity is expected to result in a
negligible impact on the affected species
or stocks. The provision requiring that
the activity not have an unmitigable
impact on the availability of the affected
species or stock for subsistence uses is
not implicated for this proposed action.
For reasons stated previously in this
document, the negligible impact
determination is supported by:
(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 fact that cetaceans would have
to be closer than 23 m (75 ft) in deep
water, 35 m (115 ft) in intermediate
depths, and 150 m (492 ft) in shallow
water when the GI airgun is in use from
the vessel to be exposed to levels of
VerDate Nov<24>2008
20:08 May 22, 2009
Jkt 217001
sound (180 dB) believed to have even a
minimal chance of causing PTS;
(3) The fact that pinnipeds would
have to closer than 8 m (26 ft) in deep
water, 12 m (39 ft) in intermediate
depths, and 95 m (312 ft) in shallow
water when the GI airgun is in use from
the vessel to be exposed to levels of
sound (190 dB) believed to have even a
minimal chance of causing PTS;
(4) The fact that marine mammals
would have to be closer than 220 m (ft)
in deep water, 330 m at intermediate
depths, and 570 m (ft) in shallow water
when the GI airgun is in use from the
vessel to be exposed to levels of sound
(160 dB) believed to have even a
minimal chance at causing TTS; and
(5) The likelihood that marine
mammal detection ability by trained
observers is high at that short distance
from the vessel, enabling the
implementation of shut-downs to avoid
injury, serious injury, or mortality. As a
result, no take by injury or death is
anticipated, and the potential for
temporary or permanent hearing
impairment is very low and will be
avoided through the incorporation of
the proposed mitigation measures.
While the number of marine
mammals potentially incidentally
harassed will depend on the
distribution and abundance of marine
mammals in the vicinity of the survey
activity, the number of potential
harassment takings is estimated to be
small, less than one percent of any of
the estimated population sizes, and has
been mitigated to the lowest level
practicable through incorporation of the
measures mentioned previously in this
document.
Proposed Authorization
As a result of these preliminary
determinations, NMFS proposes to issue
an IHA to SIO for conducting a lowenergy marine seismic survey in the
Northeast Pacific Ocean in July, 2009,
provided the previously mentioned
mitigation, monitoring, and reporting
requirements are incorporated.
Dated: March 19, 2009.
James H. Lecky,
Director, Office of Protected Resources,
National Marine Fisheries Service.
[FR Doc. E9–12149 Filed 5–22–09; 8:45 am]
BILLING CODE 3510–22–S
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DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric
Administration
RIN 0648–XP28
Incidental Taking of Marine Mammals;
Taking of Marine Mammals Incidental
to the Explosive Removal of Offshore
Structures in the Gulf of Mexico
AGENCY: National Marine Fisheries
Service (NMFS), National Oceanic and
Atmospheric Administration (NOAA),
Commerce.
ACTION: Notice; issuance of letters of
authorization.
SUMMARY: In accordance with the
Marine Mammal Protection Act
(MMPA) and implementing regulations,
notification is hereby given that NMFS
has issued one-year Letters of
Authorization (LOA) to take marine
mammals incidental to the explosive
removal of offshore oil and gas
structures (EROS) in the Gulf of Mexico.
DATES: These authorizations are
effective from June 1, 2009 through May
31, 2010.
ADDRESSES: The application and LOAs
are available for review by writing to P.
Michael Payne, Chief, Permits,
Conservation, and Education Division,
Office of Protected Resources, National
Marine Fisheries Service, 1315 EastWest Highway, Silver Spring, MD
20910–3235 or by telephoning the
contact listed here (see FOR FURTHER
INFORMATION CONTACT), or online at:
https://www.nmfs.noaa.gov/pr/permits/
incidental.htm. 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 Ken Hollingshead,
Office of Protected Resources, NMFS,
301–713–2289.
SUPPLEMENTARY INFORMATION: Section
101(a)(5)(A) of the MMPA (16 U.S.C.
1361 et seq.) directs the NMFS to allow,
upon request, the incidental, but not
intentional, taking of small numbers of
marine mammals by United States
citizens who engage in a specified
activity (other than commercial fishing)
within a specified geographical region,
if certain findings are made by NMFS
and regulations are issued. Under the
MMPA, the term ‘‘taking’’ means to
harass, hunt, capture, or kill or to
attempt to harass, hunt capture, or kill
marine mammals.
Authorization for incidental taking, in
the form of annual LOAs, may be
granted by NMFS for periods up to five
years if NMFS finds, after notification
E:\FR\FM\26MYN1.SGM
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[Federal Register Volume 74, Number 99 (Tuesday, May 26, 2009)]
[Notices]
[Pages 24799-24818]
From the Federal Register Online via the Government Printing Office [www.gpo.gov]
[FR Doc No: E9-12149]
-----------------------------------------------------------------------
DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric Administration
RIN 0648-XO71
Incidental Takes of Marine Mammals During Specified Activities;
Low-Energy Marine Seismic Survey in the Northeast Pacific Ocean, July
2009
AGENCY: National Marine Fisheries Service (NMFS), National Oceanic and
Atmospheric Administration (NOAA), Commerce.
ACTION: Notice; proposed incidental take authorization; request for
comments.
-----------------------------------------------------------------------
SUMMARY: NMFS has received an application from the Scripps Institution
of Oceanography (SIO), a part of the University of California San Diego
(UCSD), for an Incidental Harassment Authorization (IHA) to take small
numbers of marine mammals, by harassment, incidental to conducting a
marine seismic survey in the Northeast Pacific Ocean during July 2009.
Pursuant to the Marine Mammal Protection Act (MMPA), NMFS requests
comments on its proposal to authorize SIO to incidentally take, by
Level B harassment only, small numbers of marine mammals during the
aforementioned activity.
DATES: Comments and information must be received no later than June
25, 2009.
ADDRESSES: Comments on the application should be addressed to Michael
Payne, Chief, Permits, Conservation and Education Division, Office of
Protected Resources, National Marine Fisheries Service, 1315 East-West
Highway, Silver Spring, MD 20910-3225. The mailbox address for
providing email comments is PR1.0648-XO71@noaa.gov. Comments sent via
e-mail, including all attachments, must not exceed a 10-megabyte file
size.
A copy of the application containing a list of the references used
in this document may be obtained by writing to the address specified
above, telephoning the contact listed below (see FOR FURTHER
INFORMATION CONTACT), or visiting the internet at: https://www.nmfs.noaa.gov/pr/permits/incidental.htm.
[[Page 24800]]
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 Ken Hollingshead,
Office of Protected Resources, NMFS, 301-713-2289.
SUPPLEMENTARY INFORMATION:
Background
Sections 101(a)(5)(A) and (D) of the MMPA (16 U.S.C. 1361 et seq.)
direct the Secretary of Commerce to allow, upon request, the
incidental, but not intentional, taking of marine mammals 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 either regulations are issued or, if the taking
is limited to harassment, a notice of a proposed authorization is
provided to the public for review.
Authorization for incidental taking shall be granted if NMFS finds
that the taking will have a negligible impact on the species or
stock(s), will not have an unmitigable adverse impact on the
availability of the species or stock(s) for subsistence uses, and if
the permissible methods of taking and requirements pertaining to the
mitigation, monitoring and reporting of such takings are set forth.
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.
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 [ALevel 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
[ALevel B harassment@].
Section 101(a)(5)(D) establishes a 45-day time limit for NMFS=
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
comment period, NMFS must either issue or deny issuance of the
authorization.
Summary of Request
On March 9, 2009, NMFS received an application from SIO for the
taking, by Level B harassment only, of small numbers of marine mammals
incidental to conducting, under cooperative agreement with the National
Science Foundation (NSF), a low-energy marine seismic survey in the
Northeast Pacific Ocean. The funding for the survey is provided by the
NSF. The proposed survey will occur in an overall area between
approximately 44[deg] and 45[deg] N. and 124.5[deg] and 126[deg] W.
within the Exclusive Economic Zone (EEZ) of the U.S.A., and is
scheduled to occur from July 14-20, 2009. The survey will use a single
Generator Injector (GI) airgun with a discharge volume of 45 in\3\.
Some minor deviation from these dates is possible, depending on
logistics and weather.
The proposed survey is virtually identical to one conducted by SIO
in 2007 under an IHA issued in September 2007 (NMFS 2007). The proposed
SIO 2009 IHA application contains minor updates to the project
description, updated marine mammal population sizes based on the most
recent NMFS annual stock assessment, an assessment of the relevance of
the marine mammal density and distribution data contained in the SIO
2007 IHA application based on cruise reports from the NMFS SWFSC
ORCAWHALE 2008 cruise, and updated information on effects of airguns on
marine mammals (see Appendix A of SIO's application).
Description of the Specified Activity
SIO plans to conduct an ocean bottom seismograph (OBS) deployment
and a magnetic, bathymetric, and seismic survey. The planned survey
will involve one source vessel, the R/V Wecoma (Wecoma), and will occur
in the Northeast Pacific Ocean off the coast of Oregon.
The purpose of the research program is to record micro-earthquakes
in the forearc to determine whether seismicity on the plate boundary is
characteristic of a locked or a freely slipping fault plane. Several
earthquakes large enough to be recorded on land-based seismic nets have
occurred along this segment in the past several years. The occurrence
of ``repeating earthquakes'' (earthquakes with identical waveforms
indicating repeated rupture of almost the same fault patch) suggests
that this region is at a boundary between a freely slipping and a
locked portion of the fault. Some models suggest that the forearc basin
north of the seismically active zone may be locked; others suggest that
portion of the fault is slipping freely. OBSs have been deployed for a
year, and a seismic survey will be used to characterize the shallow
sediment structure around the instruments. Also, included in the
research is the use of a magnetometer and sub-bottom profiler.
The source vessel, the Wecoma, will deploy a single low-energy GI
airgun as an energy source (with a discharge volume of 45 in\3\) and a
300 m (984 ft), 16 channel, towed hydrophone streamer. Sixteen OBSs
were deployed in July and September 2008. They will continue to acquire
data during this cruise, and will be recovered before returning to
port. The energy to the GI airgun is compressed air supplied by
compressors onboard the source vessel. As the GI airgun is towed along
the survey lines, the receiving systems will receive the returning
acoustic signals.
The seismic program will consist of approximately 21 km (13 mi) of
surveys over each of the 16 OBSs (see Figure 1 of SIO's application).
Water depths at the seismic survey locations rang from just less than
100 m (328 ft) to almost 3,000 m (9,842 ft) (see Figure 1 of SIO's
application). The GI airgun will be operated on a small grid for
approximately two hours at each of the 16 OBS sites. There will be
additional seismic operations associated with equipment testing, start-
ups, and repeat coverage of any areas where initial data quality is
substandard.
All planned geophysical data acquisition activities will be
conducted by SIO with on-board assistance by the scientists who have
proposed the study. The Chief Scientist is Dr. Anne Trehu of Oregon
State University. The vessel will be self-contained, and the crew will
live aboard the vessel for the entire cruise.
In addition to the seismic operations of the single GI airgun, a
3.5 and 12 kHz sub-bottom profiler will be used continuously throughout
the cruise, and a magnetometer may be run on the transit between OBS
locations.
Vessel Specifications
The Wecoma has a length of 56.4 m (185 ft), a beam of 10.1 m (33.1
ft), and a maximum draft of 5.6 m (18.4 ft). The ship is powered by a
single 3,000-hp EMD diesel engine driving a single, controllable-pitch
propeller through a clutch and reduction gear, and an electric 350-hp
azimuthing bow thruster. An operations speed of 11.1 km/hour (6 knots)
will be used during seismic acquisition. When not towing seismic survey
gear, the Wecoma cruises at 22.2 km/hour (12 knots) and has a maximum
speed of 26 km/hour (14
[[Page 24801]]
knots). It has a normal operating range of approximately 13,300 km. The
Wecoma will also serve as the platform from which vessel-based Marine
Mammal Visual Observers (MMVO) will watch for animals before and during
GI airgun operations.
Acoustic Source Specifications
Seismic Airguns
During the proposed survey, the Wecoma will tow a single GI airgun,
with a volume of 45 in\3\, and a 300 m long streamer containing
hydrophones along predetermined lines. Seismic pulses will be emitted
at intervals of 10 seconds. At a speed of 6 knots (11.1 km/hour), the
10 second shot spacing corresponds to a shot interval of approximately
31 m (101.7 ft).
The generator chamber of the GI airgun, the one responsible for
introducing the sound pulse into the ocean, is 45 in\3\. The larger
(105 in\3\) injector chamber injects air into the previously-generated
bubble to maintain its shape, and does not introduce more sound into
the water. The 45 in\3\ GI airgun will be towed 21 m (68.9 ft) behind
the Wecoma at a depth of 4 m (13.1ft). The sound pressure field of that
GI airgun variation at a tow depth of 2.5 m has been modeled by Lamont-
Doherty Earth Observatory (L-DEO) in relation to distance and direction
for the GI airgun.
As the GI airgun is towed along the survey line, the towed
hydrophone array in the 300 m streamer receives the reflected signals
and transfers the data on the on-board processing system. Given the
relatively short streamer length behind the vessel, the turning rate of
the vessel while the gear is deployed is much higher than the limit of
five degrees per minute for a seismic vessel towing a streamer of more
typical length (much greater than 1 km). Thus, the maneuverability of
the vessel is not limited much during operations.
The root mean square (rms) received levels that are used as impact
criteria for marine mammals are not directly comparable to the peak (pk
or 0-pk) or peak-to-peak (pk - pk) values normally used to characterize
source levels of airgun arrays. The measurement units used to describe
airgun sources, peak or peak-to-peak decibels, are always higher than
the ``root mean square'' (rms) decibels referred to in biological
literature. A measured received level of 160 dB re 1 microPa (rms) in
the far field would typically correspond to a peak measurement of
approximately 170 to 172 dB, and to a peak-to-peak measurement of
approximately 176 to 178 dB, as measured for the same pulse received at
the same location (Greene, 1997; McCauley et al., 1998, 2000). The
precise difference between rms and peak or peak-to-peak values depends
on the frequency content and duration of the pulse, among other
factors. However, the rms level is always lower than the peak or peak-
to-peak level for an airgun-type source.
Received sound levels have been modeled by L-DEO for a number of
airgun configurations, including one 45 in\3\ GI airgun, in relation to
distance from the airgun(s) (see Figure 2 of SIO's application). The
model does not allow for bottom interactions, and is most directly
applicable to deep water. Based on modeling, estimates of the maximum
distances from the GI airgun where sound levels of 190, 180, and 160 dB
re 1 microPa (rms) are predicted to be received in deep (>1,000 m)
water are shown in Table 1 of SIO's application. Because the model
results are for a 2.5 m tow depth, the distances in Table 1 slightly
underestimate the distances for the 45 in\3\ GI airgun towed at 4 m
depth.
Sub-bottom Profiler
Along with the GI airgun operations, one additional acoustical data
acquisition system will be operated throughout the cruise. The ocean
floor will be mapped with a Knudsen Engineering Model 320BR 12 kHz and
3.5 kHz sub-bottom profiler (SBP). Multi-beam sonar will not be used.
The Knudsen Engineering Model 320BR SBP is a dual-frequency
transceiver designed to operate at 3.5 and/or 12 kHz. It is used to
provide data about the sedimentary features that occur below the sea
floor. The energy from the sub-bottom profiler is directed downward via
a 12 kHz transducer (EDO 323B) or a 3.5 kHz array of 16 ORE 137D
transducers in a 4x4 arrangement. The maximum power output of the 320BR
is 10 kilowatts for the 3.5 kHz section and 2 kilowatts for the 12 kHz
section.
The pulse length for the 3.5 kHz section of the 320 BR is 0.8-24
ms, controlled by the system operator in regards to water depth and
reflectivity of the bottom sediments, and will usually be 12 or 24 ms
in this survey. The system produces one sound pulse and then waits for
its return before transmitting again. Thus, the pulse interval is
directly dependent upon water depth, and in this survey is 4.5-8
seconds. Using the Sonar Equations and assuming 100 percent efficiency
in the system (impractical in real world applications), the source
level for the 320BR is calculated to be 211 dB re 1 Pam. In practical
operation, the 3.5 kHz array is seldom driven at more than 80 percent
of maximum, usually less than 50 percent.
Safety Radii
NMFS has determined that for acoustic effects, using acoustic
thresholds in combination with corresponding safety radii is an
effective way to consistently apply measures to avoid or minimize the
impacts of an action, and to quantitatively estimate the effects of an
action. Thresholds are used in two ways: (1) to establish a mitigation
shut-down or power-down zone, i.e., if an animal enters an area
calculated to be ensonified above the level of an established
threshold, a sound source is powered down or shut down; and (2) to
calculate take, in that a model may be used to calculate the area
around the sound source that will be ensonified to that level or above,
then, based on the estimated density of animals and the distance that
the sound source moves, NMFS can estimate the number of marine mammals
that may be ``taken.''
As a matter of past practice and based on the best available
information at the time regarding the effects of marine sound compiled
over the past decade, NMFS has used conservative numerical estimates to
approximate where Level A harassment from acoustic sources begins: 180
dB re 1 microPa (rms) level for cetaceans and 190 dB re 1 microPa (rms)
for pinnipeds. A review of the available scientific data using an
application of science-based extrapolation procedures (Southall et al.,
2007) strongly suggests that Level A harassment (as well as TTS) from
single sound exposure impulse events may occur at much higher levels
than the levels previously estimated using very limited data. However,
for purposes of this proposed action, SIO's application sets forth, and
NMFS is using, the more conservative 180 and 190 dB re 1 microPa (rms)
criteria. NMFS also considers 160 dB re 1 microPa (rms) as the
criterion for estimating the onset of Level B harassment from acoustic
sources like impulse sounds used in the seismic survey.
Emperical data concerning the 180 and 160 dB distances have been
acquired based on measurements during the acoustic verification study
conducted by L-DEO in the northern Gulf of Mexico from May 27 to June
3, 2003 (Tolstoy et al., 2004). Although the results are limited the
data showed that radii around the airguns where the received level
would be 180 dB re 1 microPa (rms), the safety criterion applicable to
cetaceans (NMFS, 2000), vary with water depth. Similar depth-related
variation is likely in the 190 dB distances applicable to pinnipeds.
[[Page 24802]]
Correction factors were developed for water depths 100-1,000 m and <100
m.
The empirical data indicate that, for deep water (>1,000 m), the L-
DEO model tends to overestimate the received sound levels at a given
distance (Tolstoy et al., 2004). However, to be precautionary pending
acquisition of additional empirical data, it is proposed that safety
radii during GI airgun operations in deep water will be values
predicted by L-DEO's model (see Table 1 below). Therefore, the assumed
180 and 190 dB radii are 23 m (75.5 ft) and 8 m (26 ft) respectively.
Empirical measurements indicated that in shallow water (<100 m),
the L-DEO model under estimates actual levels. In previous L-DEO
projects, the exclusion zones were typically based on measured values
and ranged from 1.3 to 15x higher than the modeled values depending on
the size of the airgun array and the sound level measured (Tolstoy et
al., 2004). During the proposed cruise, similar factors will be applied
to derive appropriate shallow water radii from the modeled deep water
radii for the GI airgun (see Table 1 below).
Empirical measurements were not conducted for intermediate depths
(100-1,000 m). On the expectation that results will be intermediate
between those from shallow and deep water, a 1.5x correction factor is
applied to the estimates provided by the model for deep water
situations. This is the same factor that was applied to the model
estimates during L-DEO cruises in 2003. The assumed 180 and 190 dB
radii in intermediate depth water are 35 m (115 ft) and 12 m (39.4 ft),
respectively (see Table 1 below).
Table 1. Predicted distances to which sound levels [gteqt]190, 180, and 160 dB re 1 microPa might be received in
shallow (<100 m; 328 ft), intermediate (100-1,000 m; 328-3,280 ft), and deep (>1,000 m; 3,280 ft) water from the
single 45 in\3\ GI airgun used during the seismic surveys in the northeastern Pacific Ocean during July 2009.
Distances are based on model results provided by L-DEO.
----------------------------------------------------------------------------------------------------------------
Predicted RMS Distances (m)
Source and Volume Tow Depth (m) Water Depth -------------------------------------
190 dB 180 dB 160 dB
----------------------------------------------------------------------------------------------------------------
Single GI airgun 45 in\3\ 4 Deep (>1,000 m) 8 23 220
----------------------------------------------
............... Intermediate (100- 12 35 330
1,000 m)
----------------------------------------------
............... Shallow (< 100 m) 95 150 570
----------------------------------------------------------------------------------------------------------------
Proposed Dates, Duration, and Region of Activity
The Wecoma is scheduled to depart from Newport, Oregon, on July 14,
2009 and to return on July 20, 2009. The GI airgun will be used for
approximately two hours at each of 16 OBS locations. The program will
consist of approximately 7 days of seismic acquisition. The exact dates
of the activities may vary by a few days because of weather conditions,
repositioning, streamer operations, and adjustments, GI airgun
deployment, or the need to repeat some lines if data quality is
substandard. The seismic surveys will take place off the Oregon coast
in the northeastern Pacific Ocean (see Figure 1 of SIO's application).
The overall area within which the seismic surveys will occur is located
between approximately 44[deg] and 45[deg] N and 124.5[deg] and 126[deg]
W (see Figure 1 of SIO's application). The surveys will take place in
water depths just less than 100 m and to almost 3,000 m, entirely
within the Exclusive Economic Zone (EEZ) of the U.S.A.
Description of Marine Mammals in the Proposed Activity Area
A total of 32 marine mammal species may occur or have been
documented to occur in the marine waters off Oregon and Washington,
excluding extralimital sightings or strandings (Fiscus and Niggol,
1965; Green et al., 1992, 1993; Barlow, 1997, 2003; Mangels and
Gerrodette, 1994; Von Saunder and Barlow, 1999; Barlow and Taylor,
2001; Buchanan et al., 2001; Calambokidis et al., 2004; Calambokidis
and Barlow, 2004). The species include 19 odontocetes (toothed
cetaceans, such as dolphins), 7 mysticetes (baleen whales), 5
pinnipeds, and sea otters. Six of the species that may occur in the
project area are listed under the Endangered Species Act (ESA) as
Endangered, including sperm, humpback, sei, fin, blue, and North
Pacific right whales. Another species, the Steller sea lion, is listed
as Threatened and may occur in the project area.
The study area is located approximately 25 to 110 km (15.5 to 68.4
mi) offshore from Oregon over water depths from just less than 100 m to
almost 3,000 m. Two of the 32 species, gray whales and sea otters, are
not expected in the project area because their occurrence off Oregon is
limited to very shallow, coastal waters. Three other species,
California sea lions, Steller sea lions, and harbor seals, are mainly
coastal, and would be rare at most at the OBS locations. Information on
the habitat, abundance, and conservation status of the species that may
occur in the study area are given in Table 2 (below, see Table 2 of
SIO's application). Vagrant ringed seals, hooded seals, and ribbon
seals have been sighted or stranded on the coast of California (see
Mead, 1981; Reeves et al., 2002) and presumably passed through Oregon
waters. A vagrant beluga whale was seen off the coast of Washington
(Reeves et al., 2002). Those seven species are not addressed in detail
in the summaries in SIO's application.
The six species of marine mammals expected to be most common in the
deep pelagic or slope waters of the project area, where most of the
survey sites are located, include the Pacific white-sided dolphin,
northern right whale dolphin, Risso's dolphin, short beaked common
dolphin, Dall's porpoise, and northern fur seal (Green et al., 1992,
1993; Buchanan et al., 2001; Barlow, 2003; Barlow and Forney, 2007;
Carretta et al., 2007). The fin whale, Dall's porpoise, and the
northern elephant seal were the species sighted most often off Oregon
and Washington during the ORCAWALE 2008 surveys (NMFS, 2008).
Table 2 below outlines the marine mammal species, their habitat,
abundance, density, and conservation status in the proposed project
area. Additional information regarding the distribution of these
species expected to be found in the project area and how the estimated
densities were calculated may be found in SIO's application.
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Potential Effects on Marine Mammals
Potential Effects of Airguns
The effects of sounds from airguns might result in one or more of
the following: tolerance, masking of natural sounds, behavioral
disturbances, temporary or permanent hearing impairment, and 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). With the possible exception of some
cases of temporary threshold shift in harbor seals, it is unlikely that
the project would result in any cases of temporary or especially
permanent hearing impairment, or any significant non-auditory physical
or physiological effects.
Tolerance
Numerous studies have shown that pulsed sounds from airguns are
often readily detectable in the water at distances of many kilometers.
For a brief summary of the characteristics of airgun pulses, see
Appendix A(3) of SIO's application. However, it should be noted that
most of the measurements are for airguns that would be detectable
considerably farther away than the GI airgun planned for use in the
present project.
Several studies have shown that marine mammals at distances more
than a few kilometers from operating seismic vessels often show no
apparent response-see Appendix A(5) of SIO's application. 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 mammal group. Although various baleen whales,
toothed whales, and (less frequently) pinnipeds have been shown to
react behaviorally to airgun pulses under some conditions, at other
times, mammals of all three types have shown no overt reactions. In
general, pinnipeds usually seem to be more tolerant of exposure to
airgun pulses than are cetaceans, with relative responsiveness of
baleen and toothed whales being variable. Given the relatively small
and low-energy GI airgun source planned for use in this project,
mammals are expected to be tolerate being closer to this source than
would be the case for a larger airgun source typical of most seismic
surveys.
Masking
Obscuring of sounds of interest by interfering sounds, generally at
similar frequencies, is known as masking. Masking effects of pulsed
sounds (even from large arrays of airguns) on marine mammal calls and
other natural sounds are expected to be limited, although there are few
specific data of relevance. Because of the intermittent nature and low
duty cycle of seismic pulses, animals can emit and receive sounds in
the relatively quiet intervals between pulses. However in some
situations, multi-path arrivals and reverberation cause airgun sound to
arrive for much or all of the interval between pulses (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. The airgun sounds are pulsed, with quiet periods between the
pulses, and whale calls often can be heard between the seismic pulses
(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). In the northeast Pacific Ocean, blue whale calls have been
recorded during a seismic survey off Oregon (McDonald et al., 1995).
Among odontocetes, there has been one report that sperm whales cease
calling when exposed to pulses from a very distant seismic ship (Bowles
et al., 1994). However, more recent studies found that sperm whales
continued calling in the presence of seismic pulses (Madsen et al.,
2002; Tyack et al., 2003; Smultea et al., 2004; Holst et al., 2006;
Jochens et al., 2006, 2008). Given the small source planned for use
during the proposed survey, there is even less potential for masking of
baleen or sperm whale calls during the present study than in most
seismic surveys. Masking effects of seismic pulses are expected to be
negligible in the case of the small odontocetes given the intermittent
nature of seismic pulses. Dolphins and porpoises commonly are heard
calling while airguns are operating (Gordon et al., 2004; Smultea et
al., 2004; Holst et al., 2005a,b; Potter et al., 2007). Also, the
sounds important to small odontocetes are predominantly at much higher
frequencies than the airgun sounds, thus further limiting the potential
for masking. In general, masking effects of seismic pulses are expected
to be minor, given the normally intermittent nature of seismic pulses.
Masking effects on marine mammals are discussed further in Appendix A
(4) of SIO's application.
Disturbance Reactions
Disturbance includes a variety of effects, including subtle changes
in behavior, more conspicuous changes in activities, 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. If a marine mammal responds to an underwater sound by
changing its behavior or moving a small distance, the response may or
may not rise to the level of ``harassment,'' or affect the stock or the
species as a whole. However, if a sound
[[Page 24806]]
source displaces marine mammals from an important feeding or breeding
area for a prolonged period, impacts on animals or on the stock or
species could potentially be significant (Lusseau and Bejder, 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 are likely to be present within a particular distance
of industrial activities, or exposed to a particular level of
industrial sound. This practice potentially overestimates the numbers
of marine mammals that are affected in some biologically-important
manner.
The sound exposure thresholds that are used to estimate how many
marine mammals might be harassed by a seismic survey are based on
behavioral observations during studies of several species. However,
information is lacking for many species. Detailed studies have been
done on humpback, gray, bowhead, and on ringed seals. Less detailed
data are available for some other species of baleen whales, sperm
whales, small toothed whales, and sea otters, but for many species
there are no data on responses to marine seismic surveys. Most of those
studies have concerned reactions to much larger airgun sources than
planned for use in the proposed project. Thus, effects are expected to
be limited to considerably smaller distances and shorter periods of
exposure in the present project than in most of the previous work
concerning marine mammal reactions to airguns.
Baleen Whales - Baleen whales generally tend to avoid operating
airguns, but avoidance radii are quite variable. 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, as reviewed in Appendix A(5) of SIO's application,
baleen whales exposed to strong noise pulses from airguns often react
by deviating from their normal migration route and/or interrupting
their feeding activities and moving away from the sound source. In the
case of the migrating gray and bowhead whales, the observed changes in
behavior appeared to be of little or no biological consequence to the
animals. 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 demonstrated
that received levels of pulses in the 160-170 dB re 1 microPa rms range
seem to cause obvious avoidance behavior in a substantial fraction of
the animals exposed. In many areas, seismic pulses from large arrays of
airguns diminish to those levels at distances ranging from 4.5-14.5 km
(2.8-9 mi) from the source. A substantial proportion of the baleen
whales within those distances may show avoidance or other strong
disturbance reactions to the airgun array. Subtle behavioral changes
sometimes become evident at somewhat lower received levels, and studies
summarized in Appendix A(5) of SIO's application have shown that some
species of baleen whales, notably bowhead and humpback whales, at times
show strong avoidance at received levels lower than 160-170 dB re 1
microPa (rms). Reaction distances would be considerably smaller during
the proposed project, for which the 160 dB radius is predicted to be
220 to 570 m (722 to 1,870 ft) (see Table 1 above), as compared with
several km when a large array of airguns is operating.
Responses of humpback whales to seismic surveys have been studied
during migration, on the summer feeding grounds, and on Angolan winter
breeding grounds; there has also been discussion of effects on the
Brazilian wintering grounds. McCauley et al. (1998, 2000a) studied the
responses of humpback whales off Western Australia to a full-scale
seismic survey with a 16-airgun, 2,678 in\3\ array, and to a single 20
in\3\ airgun with a source level of 227 dB re 1 microPa m peak-to-peak.
McCauley et al. (1998) documented that initial avoidance reactions
began at 5 to 8 km (3.1 to 5 mi) from the array, and that those
reactions kept most pods approximately 3 to 4 km (1.9 to 2.5 mi) from
the operating seismic boat. McCauley et al. (2000) noted localized
displacement during migration of 4 to 5 km (2.5 to 3.1 mi) by traveling
pods and 7 to12 km (4.3 to 7.5 mi) by cow-calf pairs. Avoidance
distances with respect to the single airgun were smaller (2 km (1.2
mi)) but consistent with the results from the full array in terms of
received sound levels. The mean received level for initial avoidance
reactions of an approaching airgun was a sound level of 140 dB re 1
microPa (rms) for humpback whale pods containing females. The standoff
range, i.e., the closest point of approach (CPA) of the whales to the
airgun, corresponded to a received level of 143 dB re 1 microPa (rms).
The initial avoidance response generally occurred at distances of 5 to
8 km (3.1 to 5 mi) from the airgun array and 2 km (1.2 mi) 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 microPa (rms).
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 150-169 dB re 1 microPa on an
approximate rms basis. 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 re 1 microPa on an approximate rms basis.
Among wintering humpback whales off Angola (n = 52 useable groups),
there were no significant differences in encounter rates (sightings/hr)
when a 24 airgun array (3,147 in\3\ or 5,805 in\3\) was operating vs.
silent (Weir, 2008). There was also no significant difference in the
mean CPA distance of the humpback whale sightings when airguns were on
vs. off (3,050 m vs. 2,700 m or 10,007 vs. 8,858 ft, respectively).
It has been 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 results from 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, 2007b:236).
There are no data on reactions of right whales to seismic surveys,
but results from the closely-related bowhead whale show that their
responsiveness can be quite variable depending on the activity (e.g.,
migrating vs. feeding). Bowhead whales migrating west across the
Alaskan Beaufort Sea in autumn, in particular, are unusually
responsive, with substantial avoidance occurring out to distances of
20-30 km (12.4-18.6 mi) from a medium-sized airgun source at received
sound levels of around 120-130 dB re 1 microPa (rms) (Miller et al.,
1999; Richardson et al., 1999; see Appendix B (5) of L-DEO's
application). However, more recent research on bowhead whales (Miller
et al., 2005a; Harris et al., 2007) corroborates earlier evidence that,
during the summer feeding season, bowheads are not as sensitive to
seismic sources. Nonetheless, subtle but statistically significant
changes in surfacing-respiration-dive cycles were evident
[[Page 24807]]
upon statistical analysis (Richardson et al., 1986). In summer,
bowheads typically begin to show avoidance reactions at a received
level of about 160-170 dB re 1 microPa (rms) (Richardson et al., 1986;
Ljungblad et al., 1988; Miller et al., 2005a).
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. Malme et al. (1986, 1988) estimated, based on small sample sizes,
that 50 percent of feeding gray whales ceased feeding at an average
received pressure level of 173 dB re 1 microPa on an (approximate) rms
basis, and that 10 percent of feeding whales interrupted feeding at
received levels of 163 dB. 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 with observations of Western Pacific
gray whales feeding off Sakhalin Island, Russia, when a seismic survey
was underway just offshore of their feeding area (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). Gray whales
typically show no conspicuous responses to airgun pulses with received
levels up to 150 to 160 dB re 1 microPa (rms), but are increasingly
likely to show avoidance as received levels increase above that range.
Various species of Balaenoptera (blue, sei, fin, Bryde's, and minke
whales) have occasionally been reported in areas ensonified by airgun
pulses (Stone, 2003; MacLean and Haley, 2004; Stone and Tasker, 2006).
Sightings by observers on seismic vessels off the United Kingdom from
1997 to 2000 suggest that, at times of good sightability, sighting
rates for mysticetes (mainly fin and sei whales) were similar when
large arrays of airguns were shooting and not shooting (Stone, 2003;
Stone and Tasker, 2006). However, these whales tended to exhibit
localized avoidance, remaining significantly (on average) from the
airgun array during seismic operations compared with non-seismic
periods (Stone and Tasker, 2006). In a study off Nova Scotia, Moulton
and Miller (2005) found little difference in sighting rates (after
accounting for water depth) and initial sighting distances of
balaenopterid whales when airguns were operating vs. silent. However,
there were indications that these whales were more likely to be moving
away when seen during airgun operations. Similarly, ship-based
monitoring studies of blue, fin, sei, and minke whales offshore of
Newfoundland (Orphan Basin and Laurentian Sub-basin) found no more than
small differences in sighting rates and swim direction during seismic
vs. non-seismic periods (Moulton et al., 2005, 2006a,b).
Data on short-term reactions (or lack of reactions) of cetaceans to
impulsive noises do not necessarily provide information about long-term
effects. It is not known whether impulsive noises affect reproductive
rate or distribution and habitat use in subsequent days or years.
However, gray whales 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 (see Appendix A in Malme et al., 1984;
Richardson et al., 1995; Angliss and Outlaw, 2008). The Western Pacific
gray whale population did not seem affected by a seismic survey in its
feeding ground during a prior year (Johnson et al., 2007). Bowhead
whales 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).
In any event, brief exposures to sound pulses from the proposed airgun
source are highly 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, systematic studies on sperm
whales have been done (Jochens and Biggs, 2003; Tyack et al., 2003;
Jochens et al., 2006; Miller et al., 2006), and there is an increasing
amount of information about responses of various odontocetes to seismic
surveys based on monitoring studies (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; Weir, 2008).
Seismic operators and MMOs on seismic vessels regularly see
dolphins and other small toothed whales near operating airgun arrays,
but in general there seems to be a tendency for most delphinids to show
some avoidance of operating seismic vessels (Goold, 1996a,b,c;
Calambokidis and Osmek, 1998; Stone, 2003; Moulton and Miller, 2005;
Holst et al., 2006; Stone and Tasker, 2006; Weir, 2008). 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 airgun arrays are
firing (Moulton and Miller, 2005). Nonetheless, there have been
indications that small toothed whales sometimes 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 (Stone and Tasker,
2006; Weir, 2008). In most cases, the avoidance radii for delphinids
appear to be small, on the order of 1 km (0.62 mi) or less, and some
individuals show no apparent avoidance. The beluga is a species that
(at least at times) shows long-distance avoidance of seismic vessels.
Aerial surveys during seismic operations in the southeastern Beaufort
Sea during summer recorded much lower sighting rates of beluga whales
within 10-20 km (6.2-12.4 mi) compared with 20-30 km (mi) from an
operating airgun array, and observers on seismic boats in that area
rarely see belugas (Miller et al., 2005a; Harris et al., 2007).
Captive bottlenose dolphins and beluga whales 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; Finneran and Schlundt, 2004). The animals tolerated high received
levels of sound (pk-pk level >200 dB re 1 microPa) before exhibiting
aversive behaviors. For pooled data at 3, 10, and 20 kHz, sound
exposure levels during sessions with 25, 50, and 75 percent altered
behavior were 180, 190, and 199 dB re 1 microPa\2\, respectively
(Finneran and Schlundt, 2004).
Results for porpoises depend on species. Dall's porpoises seem
relatively tolerant of airgun operations (MacLean and Koski, 2005) and,
during a survey with a large airgun array, tolerated higher noise
levels than did harbor porpoises and gray whales (Bain and Williams,
2006). However, Dall's porpoises do respond to the approach of large
airgun arrays by moving away (Calambokidis and Osmek, 1998; Bain and
Williams, 2006). The limited available data suggest that harbor
porpoises show stronger avoidance (Stone, 2003; Bain and Williams,
2006; Stone and Tasker, 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
in general (Richardson et al., 1995; Southall et al. 2007).
[[Page 24808]]
Most studies of sperm whales exposed to airgun sounds indicate that
this species shows considerable tolerance of airgun pulses (Stone,
2003; Moulton et al., 2005, 2006a; Stone and Tasker, 2006; Weir, 2008).
In most cases, the whales do not show strong avoidance and continue to
call (see Appendix A in SIO's application). However, controlled
exposure experiments in the Gulf of Mexico indicate that foraging
effort is somewhat altered upon exposure to airgun sounds (Jochens et
al., 2006, 2008). In the SWSS study, D-tags (Johnson and Tyack, 2003)
were used to record the movement and acoustic exposure of eight
foraging sperm whales before, during, and after controlled sound
exposures of airgun arrays in the Gulf of Mexico (Jochens et al.,
2008). Whales were exposed to maximum received sound levels between 111
and 147 dB re 1 microPa (rms) (131 to 164 dB re 1 microPa pk-pk) at
ranges of approximately 1.4 to 12. 6 km (0.9 to 7.8 mi) from the sound
source. Although the tagged whales showed no horizontal avoidance, some
whales changed foraging behavior during full array exposure (Jochens et
al., 2008).
There are almost no specific data on the behavioral reactions of
beaked whales to seismic surveys. However, northern bottlenose whales
(Hyperodon ampullatus) continued to produce high-frequency clicks when
exposed to sound pulses from distant seismic surveys (Laurinolli and
Cochrane, 2005; Simard et al., 2005). Most beaked whales tend to avoid
approaching vessels of other types (Wursig et al., 1998). They may also
dive for an extended period when approached by a vessel (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 quire long
(Baird et al., 2006; Tyack et al., 2006). In any event, it is likely
that these beaked whales would normally show strong avoidance of an
approaching seismic vessel, but this has not been documented
explicitly.
Odontocete reactions to large arrays of airguns are variable and,
at least for delphinids and Dall's porpoises, seem to be confined to a
smaller radius than has been observed for the more responsive of the
mysticetes, belugas, and harbor porpoises (Appendix A of SIO's
application).
Additional details on the behavioral reactions (or the lack
thereof) by all types of marine mammals to seismic vessels can be found
in Appendix A(5) of SIO's application.
Hearing Impairment and Other Physical Effects
Temporary or permanent hearing impairment is a possibility when
marine mammals are exposed to very strong sounds, but there has been no
specific documentation of this for marine mammals exposed to sequences
of airgun pulses.
NMFS will be developing new noise exposure criteria for marine
mammals that take account of the now-available scientific data on
temporary threshold shift (TTS), the expected offset between the TTS
and permanent threshold shift (PTS) thresholds, differences in the
acoustic frequencies to which different marine mammal groups are
sensitive, and other relevant factors. Detailed recommendations for new
science-based noise exposure criteria were published in late 2007
(Southall et al., 2007).
Several aspects of the planned monitoring and mitigation measures
for this project (see below) are designed to detect marine mammals
occurring near the airguns to avoid exposing them to sound pulses that
might, at least in theory, cause hearing impairment. In addition, many
cetaceans and (to a limited degree) pinnipeds are likely to show some
avoidance of the area where received levels of airgun sound are high
enough such that hearing impairment could potentially occur. In those
cases, the avoidance responses of the animals themselves will reduce or
(most likely) avoid any possibility of hearing impairment.
Non-auditory physical effects may also occur in marine mammals
exposed to strong underwater pulsed sound. Possible types of non-
auditory physiological effects or injuries that theoretically might
occur in mammals close to a strong sound source include stress,
neurological effects, bubble formation, resonance effects, and other
types of organ or tissue damage. It is possible that some marine mammal
species (i.e., beaked whales) may be especially susceptible to injury
and/or stranding when exposed to strong pulsed sounds. However, as
discussed below, there is no definitive evidence that any of these
effects occur even for marine mammals in close proximity to large
arrays of airguns. It is especially unlikely that any effects of these
types would occur during the present project given the brief duration
of exposure of any given mammal and the proposed monitoring and
mitigation measures (see below). The following subsections discuss in
somewhat more detail the possibilities of TTS, PTS, and non-auditory
physical effects.
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).
For toothed whales exposed to single short pulses, the TTS
threshold appears to be, to a first approximation, a function of the
energy content of the pulse (Finneran et al., 2002, 2005). Given the
available data, the received level of a single seismic pulse (with no
frequency weighting) might need to be approximately 186 dB re 1
microPa\2\\.\s (i.e., 186 dB SEL or approximately 221-226 dB pk-pk) in
order to produce brief, mild TTS. Exposure to several strong seismic
pulses that each have received levels near 190 dB re 1 microPa (rms)
(175-180 dB SEL) might result in cumulative exposure of approximately
186 dB SEL and thus slight TTS in a small odontocete, assuming the TTS
threshold is (to a first approximation) a function of the total
received pulse energy. Levels [gteqt] 190 dB 1 microPa (rms) are
expected to be restricted to radii no more than 95 m (312 ft) from the
Wecoma's GI airgun. For an odontocete closer to the surface, the
maximum radius with [gteqt]190 dB 1 microPa (rms) would be smaller.
The above TTS information for odontocetes is derived from studies
on the bottlenose dolphin and beluga. There is not published TTS
information for other species of cetaceans. However, preliminary
evidence from harbor porpoise exposed to airgun sound suggests that its
TTS threshold may have been lower (Lucke et al., 2007).
For baleen whales, there are no data, direct or indirect, on levels
or properties of sound required to induce TTS. The frequencies to which
baleen whales are most sensitive are lower than those for odontocetes,
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)
[[Page 24809]]
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. In any event, no cases
of TTS are expected given three considerations:
(1) Small size of the GI airgun source;
(2) The strong likelihood that baleen whales would avoid the
approaching airguns (or vessel) before being exposed to levels high
enough for TTS to possibly occur; and
(3) The mitigation measures that are planned.
In pinnipeds, TTS thresholds associated with exposure to brief
pulses (single or multiple) of underwater sound have not been measured.
Initial evidence from prolonged (non-pulse) exposures suggested that
some pinnipeds may incur TTS at somewhat lower received levels than do
small odontocetes exposed for similar durations (Kastak et al., 1999,
2005; Ketten et al., 2001; Au et al., 2000). The TTS threshold for
pulsed sounds has been indirectly estimated as being an SEL of
approximately 171 dB re 1 microPa2.s (Southall et al.,
2007), which would be equivalent to a single pulse with received level
approximately 181-186 re 1 microPa (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 are likely to be
higher (Kastak et al., 2005).
A marine mammal within a radius of less than 100 m (328 ft) around
a typical large array of operating airguns might be exposed to a few
seismic pulses with levels of greater than or equal to 205 dB, and
possibly more pulses if the mammal moved with the seismic vessel. (As
noted above, most cetacean species tend to avoid operating airguns,
although not all individuals do so.) In addition, ramping up airgun
arrays, which is standard operational protocol for large airgun arrays
and proposed for this action, should allow cetaceans to move away form
the seismic source and avoid being exposed to the full acoustic output
of the airgun array. Even with a large airgun array, it is unlikely
that the cetaceans would be exposed to airgun pulses at a sufficiently
high level for a sufficiently long period to cause more than mild TTS,
given the relative movement of the vessel and the marine mammal. The
potential for TTS is much lower in this project. With a large array of
airguns, TTS would be most likely in any odontocetes that bow-ride or
otherwise linger near the airguns. While bow-riding, odontocetes would
be at or above the surface, and thus not exposed to strong pulses given
the pressure-release effect at the surface. However, bow-riding animals
generally dive below the surface intermittently. If they did so while
bow-riding near airguns, they would be exposed to strong sound pulses,
possibly repeatedly. If some cetaceans did incur TTS through exposure
to airgun sounds, this would very likely be mild, temporary, and
reversible.
To avoid the potential for injury, NMFS has determined that
cetaceans and pinnipeds should not be exposed to pulsed underwater
noise at received levels exceeding, respectively, 180 and 190 dB re 1
microPa (rms). As summarized above, data that are now available imply
that TTS is unlikely to occur unless odontocetes (and probably
mysticetes as well) are exposed to airgun pulses stronger than 180 dB
re 1 microPa (rms).
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, while 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 TTS, there has been further speculation about the
possibility that some individuals occurring very close to airguns might
incur PTS (Richardson et al., 1995). Single or occasional occurrences
of mild TTS are not indicative of permanent auditory damage.
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. PTS might occur at a received sound level at
least several decibels above that inducing mild TTS if the animal were
exposed to strong sound pulses with rapid rise time (see Appendix A(5)
of SIO's application). 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
>6 dB (Southall et al., 2007). On an SEL basis, Southall et al. (2007)
estimated that received levels would need to exceed the TTS threshold
by at least 15 dB for there to be risk of PTS. Thus, for cetaceans they
estimate that the PTS threshold might be an M-weighted SEL (for the
sequence of received pulses) of approximately 198 dB re 1
microPa\2\micros (15 dB higher than the TTS threshold for an impulse).
Additional assumptions had to be made to derive a corresponding
estimate for pinnipeds, as the only available data on TTS thresholds in
pinnipeds pertain to non-impulse sound. Southall et al. (2007) estimate
that the PTS threshold could be a cumulative Mpw-weighted SEL of
approximately 186 dB 1 microPa\2\\.\s in the harbor seal to impulse
sound. The PTS threshold for the California sea lion and northern
elephant seal the PTS threshold would probably be higher, given the
higher TTS thresholds in those species.
Southall et al. (2007) also note that, regardless of the SEL, there
is concern about the possibility of PTS if a cetacean or pinniped
receives one or more pulses with peak pressure exceeding 230 or 218 dB
re 1 microPa (3.2 bar\.\ m, 0-pk), which would only be found within a
few meters of the largest (600-in\3\) airguns in the planned airgun
array (Caldwell and Dragoset, 2000). A peak pressure of 218 dB re 1
microPa could be received somewhat farther away; to estimate that
specific distance, one would need to apply a model that accurately
calculates peak pressures in the near-field around an array of airguns.
Given the higher level of sound necessary to cause PTS as compared
with TTS, it is considerably less likely that PTS could occur. Baleen
whales generally avoid the immediate area around operating seismic
vessels, as do some other marine mammals. The planned monitoring and
mitigation measures, including visual monitoring and shut downs of the
airguns when mammals are seen about to enter or within the proposed
exclusion zone (EZ), will further reduce the probability of exposure of
marine mammals to sounds strong enough to induce PTS, see the section
below on Proposed Mitigation and Monitoring.
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 effects, and other types of organ
or tissue damage (Cox et al., 2006; Southall et al., 2007). Studies
examining such effects are limited. However, resonance (Gentry, 2002)
and direct noise-induced bubble formation (Crum et al., 2005) are not
expected in the case of an impulsive 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
[[Page 24810]]
specific evidence of this upon exposure to airgun pulses.
In general, little is known about the potential for seismic survey
sounds to cause auditory impairment or other physical effects in marine
mammals. Available data suggest that such effects, if they occur at
all, would presumably be limited to short distances from the sound
source 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 auditory impairment or non-auditory
physical effects. Also, the planned mitigation measures, including shut
downs of the airgun, would reduce any such effects that might otherwise
occur.
Strandings and Mortality
Marine mammals close to underwater detonations of high explosives
can be killed or severely injured, and their auditory organs are
especially susceptible to injury (Ketten et al., 1993; Ketten, 1995).
However, explosives are no longer used for marine seismic research or
commercial seismic surveys, and have been replaced entirely by airguns
or related non-explosive pulse generators. Airgun pulses are less
energetic and have slower rise times, and there is no specific evidence
that they can cause injury, death, or stranding even in the case of
large airgun arrays. However, the association of mass strandings of
beaked whales with naval exercises and, in one case, an L-DEO seismic
survey (Malakoff, 2002; Cox et al., 2006), has raised the possibility
that beaked whales exposed to strong ``pulsed'' sounds may be
especially susceptible to injury and/or behavioral reactions that can
lead to stranding (Hildebrand, 2005; Southall et al., 2007). Appendix
A(5) of SIO's application provides additional details.
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 hemorrahage or other forms of trauma;
(3) A physiological change such as a vestibular response leading to
a behavioral change or stress-induced hemorrahagic 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.
As noted in SIO's application, some of these mechanisms are
unlikely to apply in the case of impulse sounds. However, there are
increasing indications that gas-bubble disease (analogous to ``the
bends''), induced in super-saturated tissue by a behavioral response to
acoustic exposure, could be 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 pulses 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 with most of the energy below 1
kHz. Typical military mid-frequency sonars operate at frequencies of 2-
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 assume that there is a direct connection
between the effects of military sonar and seismic surveys on marine
mammals. However, evidence that sonar pulses can, in special
circumstances, lead (at least indirectly) to physical damage and
mortality (Balcomb and Claridge, 200