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ARCTIC
VOL. 40, NO. 1 (MARCH 1987) P. 33-42
Aerial Surveys for Cetaceans in the Former Akutan, Alaska, Whaling Grounds
B.S. STEWART,’ S.A. KARL,’ P.K. YOCHEM,’ S . LEATHERWOOD’ and J.L. LAAKE’
(Received 5 June 1985; accepted in revised form 7 August 1986)
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ABSTRACT. Randomized aerial surveys were flown between 26 July and 26August 1984 to search for cetaceans in two areas of southwestern Alaska:
one on both Bering Sea and Pacific Ocean sides of the Aleutian Islands near the defunct Akutan shore-whaling station, which operated from 1912 through
1939, the other overlapping continental slope and shallow continental shelf waters between the Aleutians and the Pribilof Islands. Surveys were made at
altitudes between about 150 m and 245 m from a Partenavia P68 Observer with a plexiglass nose bubble, which permitted center-line viewing. Searches
covered about 3940 nautical miles (nm), including some 2403 nm of random transects. Sightings were made of gray whales (10 sightings, 14
individuals), fin whales (3, 1 l), minke whales (1, l), unidentified beaked whales ( I , 6), Dall’s porpoises (47, 131), killer whales (8, 26), and harbor
porpoises (4,7). A Fourier series model was used to estimate density of Dall’s porpoises as 115 individuals (CV = 0.263) per 1000 nm2 on the whaling
grounds and 16.6 individuals (CV=O.O) per lo00 n m 2 in the Bering Sea north of the whaling grounds. These estimates are comparable to those
previously reported for the same general areas (97.2 animals per lo00 nm2, SD=49.5). There were too few sightings of other cetaceans to permit
calculation of meaningful density estimates. At least four species of great whales (blue, fin,humpback and sperm) were sufficiently abundant during the
first four decades of this century to support significant whaling activities within about 100 nm of Akutan (more than 5300 whales were caught during 23
years of whaling, 1912-39). Although previous studies of the fisheries showed a downward trend in catch per unit of effort and an increase in distance
traveled to take whales, whales were still being taken at relatively high rates (0.28-0.51 whales per gross catcher day) at the end of the fishery in 1939.
Populations of fin, humpback, blue and sperm whales were probably significantly reduced by shore and pelagic whaling conducted widely in the North
Pacific since 1939. The low number of sightings on the present surveys probably means that populations on and near the whaling grounds remain
depressed from such activities.
Key words: aerial surveys, cetaceans, Bering Sea, North Pacific Ocean, historical whaling
RÉSUMÉ. Des relevis aeriens ont étt effectues au hasard entre le 26 juillet etle 26 août 1984, afin de determiner la presence de cetacts dansdeux régions
du Sud-Ouest de l’Alaska: l’une située des deux côtes des îles Aldoutiennes (du côte dela mer de Bering et du côté del’océan Pacifique), près de ce qui
fut jadisle port baleinier d’Akukan qui resta en op6ration de 1912 à 1939; l’autre couvrantà la fois les eaux du talus continental et celles,peu profondes,
de la plate-forme continentale, entre les îles Aleoutiennes et les îles Pribilof. Les relevds furent effectues à des altitudes comprises entre 150 et 245 m,
d’un appareil d’observation Partenavia P68, muni d’un nez de plexiglas, permettant de voir dans l’axe de déplacement. Les recherches ont été effectuees
sur environ 3940 milles nautiques (mn), y compris 2403 mn de recoupements au hasard. On a relev6 la presence de baleines grises (10 relevés, 14
individus),derorqualscommuns(3, ll),depetitsrorquals(l, l),debaleinesàbecnonidentifi6es(l,6),demarsouinsdeDal1(47,131),d’épaulards(8,
26) et demarsouins communs. On a utilise un modble en series de Fourier pour determiner approximativement la densit6 de marsouins de Dall à 115
individus (CV = 0.263) aux 1000
dans les zones de pêche à l a baleine, età 16.6 individus (CV = 0.0) aux lo00 mnz dans la mer de B6ring au nord
des zones de pêche. Ces evaluations sont comparables à celles rapportees prkcedemment pour ces mêmes zones en gbnéral(97.2animaux aux 1000 m2,
DS = 49.5). Troppeu d’autres cetaces ont et6 aperçus pour justifier le calcul des densites approximatives. Durant les quarante premitres années de ce
siècle, ily avait au moins quatre espi?ces de grandes baleines (rorquals bleus, rorquals communs, rorqualsàbosse et cachalots) en quantité suffisante pour
alimenter une industrie baleinibre dans un rayon d’environ 100 mn d’Akutan. (Plus de 5300 aleines furent pêchees durant les 23 années que dura la
pêche àla baleine, de 1912 1939). Bien que des etudes pdcedentes sur la pêche aient montr ne tendance à la baisse du nombre de prises par rapport au
nombre d’unitésd’effort et une augmentation de la distance à parcourir pour capturer les baleines,,celles-ci étaient captudes àun taux relativement élevé
(de 0.28 à 0.51 baleine par unit6 d’effort brute par jour) à la fin de la pêche en 1939. Les populations de rorquals communs, de rorquals à bosse, de
rorquals bleus et de cachalots ont probablement eté dduites de façonsignificative par le pêche côtibre et la pêche pélagique, qui ont et6 pratiqu6es à
grande tchelle dansle Pacifique Nord depuis 1939. Le petit nombre de cetacCs aperçus durant les présents relevds porte àcroire queles populations dans
les zones de pêche et dans leur vicinite, restent peu Blevees en raison de ces activitts.
Mots clés: relevé aerien, cetacts, mer de Bering, Pacifique Nord, ancienne pêche à la baleine
Traduit pour le journal par N6sida Loyer.
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A
INTRODUCTION
Between 1912 and 1939 whaling operations were conducted
from a shore station on Akutan Island, in the eastern Aleutian
Islands, Alaska (Fig. 1). Between May andOctober in the years
1912, 1914-20, 1922-30 and 1934-39 two to seven vessels
hunted whales within anapproximately 100 nautical mile (nm)
radius of the station on both BeringSea and Pacific Ocean sides
of the Aleutian Islands and in Unimak Pass. Catches consisted
mainly of fin (Bulaenopteraphysalus) (at least 2498), humpback (Meguprera novaeangliae) (15 lo), blue (B. musculus)
(835) and sperm (Physeter catodon) (482) whales, with occasional takesof right whales (Eubalaena glacialis)(9) and other
species (Reeves et al., 1985). Trends in availability to the
whalers of the four key species within andamong years (Leatherwood et al., 1985), interpreted in the context of other data
available for the area (Leatherwood et al., 1983), suggest that:
1) Finwhales formerly were present on both sides of the
Aleutian Islands chain from April through early September. In
July and August they were found primarily in the Bering Sea,
where they wererelatively abundant nearUnalaska and Akutan
islands. The southeast Bering Sea apparently was animportant
spring-summer feeding ground. By Augustor early September,
the population center had shifted to the North Pacific. Migration
between the two areas apparently concentrated in Unimak and
Akutan passes. 2) Humpback whales were present in greatest
numbers from June through August, in the Pacific, in Unimak
Pass and inthe Bering Sea just north of the pass. 3) Blue whales
were most abundant from June through August, almost exclusively on the Pacific side of the islands. 4) Sperm whales, all
adult males, were found in the Pacific near Akutan Island and
rarely in the Bering Sea, largely in July.
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‘Sea World Research Institute, Hubbs Marine Research Center, 1700 South Shores Road, San Diego, California 92109, U.S.A.
’San Diego State University, San Diego, California 92182, U.S.A.
@The Arctic Institute of North America
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34
B . S . STEWART er al.
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Southwestern Alaskaand the eastern Aleutian Islands, showing the location of the shore whaling stationon Akutan and the threeblocks in which transects
were flown. The adjoining photos show the station in about 1920 (lower right) and the site in early August 1984 (to left). (Photos courtesy of Alaska Historical
Library, Juneau, bottom, and by S.A. Karl, top.)
FIG. 1.
Analysis of trends in the Akutan
fishery (Leatherwood et al.,
1985)indicatedsome depletion of the stocks. Both fin and
humpbackwhalesweretaken
at greater distances from the
station in later than inearlier yeiirs, indicating reduced availability. Overall, there was a downward trend of catch per unit of
effort, also taken to meanstockswere declining somewhat.
Nevertheless, significant numbers of whales apparently were
still available to the whalers between 1935 and 1939, as 0.280.51 whales per gross catcher day were taken in the last five
years of operation. Whaling continued in the North Pacific after
the closure of the Akutan station in 1939, and it is generally
accepted that subsequent intense episodes of whaling in the
northeastern Pacific from shore stations and pelagic fleets left
most great whale stocks in the broader area depressed (e.g.,
Rice, 1974; Tillman, 1977; Braham, 1984).
In 1982 and 1983, a series of eight aerial surveys of the
southeastern Bering Sea and Bristol Bay (Ca. 185 O00 nm2) was
flown to determine geographic and seasonal distribution and
relative abundance of cetaceans. The transect lines in this
enormous area werewidelyspacedand
covered only about
1.93% of the areas during each survey. Furthermore, surveys
were often flown in less than ideal survey conditions (see
Leatherwood et al., 1983:Table 2, p. 9 and Table 4, p. 42).
With the exception of gray whales (Eschrichtius robustus),for
which it was possible
to estimate density in portions of the
southeastern Bering Sea in May andJune (Leatherwood et al.,
1983:Table 10, p. 67), few great whales were seen (Leatherwood
et al., 1983:Table 7, p.57). Several hypotheses were proposed
to explain the apparent low density of whales in the area overall,
and particularly in the
portions of the surveyed area where some
species formerly occurred in muchgreater abundance: 1) it was
an artifact of sparse coverage and generally poor survey conditions; 2) whale distribution was highlylocalized near the Aleutian Islands where previous whaling
effort had concentrated, but
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CETACEANS OFF SOUTHWESTERN ALASKA
where aerial survey coverage was low; and 3) there were few
great whales present in the eastern Bering Sea during survey
periods in 1982 and 1983.
To testthese hypotheses, in 1984 we flew intensive lowaltitude aerial surveysof the former Akutan whalinggrounds at
preciselythetime of yearwhen the greatest abundance of
whaleswasexpectedon
the grounds, as determined from
historical whaling records (see Reeves et al., 1985). We also
flew a smaller number of transects in an area straddling the
continental slope between the whalinggrounds and the Pribilof
Islands, near scheduled oil and gas exploration and developments.
35
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METHODS
Survey Design, Transect Selection and Placement
Surveys were designed using a stratified random sampling
scheme to balance the need for a random sample with practical
logistical and operational constraints. The former whaling
grounds, defined by reference to Reeves et al. (1985:Figs. 11
and 12), were divided into two blocks, one south (block 1) and
one north (block 2) of the Aleutian Islands chain but with a
common southwest to northeast oriented boundary between
them (Fig. 1). Blocks 1 and 2 covered about 14 400 nm2. Each
block was subdividedinto three zonesof equal width. The sizes
of blocks andzoneswere defined suchthat the amount of
searching in each zone or combination of zones for which
density estimates were to be reported (i.e., blocks 1 and 2
collectively and block 3 alone) was roughly proportional to its
area. This feature permitted blocks and zones to be combined
for density estimates.
The boundary between blocks1 and 2 was scored at 0.25 nm
intervals. Before beginningsurveys, eight sets of three numbers
each were selected at random and without replacement. These
represented the starting points of 48 transects (24 in each block,
8 in each zone) to be flown northwest
to southeast or southeast to
northwest, parallel to the zones’ long boundaries.
A third block (block 3) was defined between Unimak Pass
and the Pribilof Islands, in waters overlapping coastal, continental shelf and pelagic areas (Fig. 1) in which at least fin, sei
(B. borealis), minke (B. acutorostrata), humpback, gray, right
and bowhead (Baluena mysticetus) whales and various other
smaller cetaceans had been reported recently (Leatherwood et
al., 1983). This rectangular block, which covered 4000 nm2,
was divided into two zones, each approximately 20 X 100 nm.
The westernmargin of each zone was scored at 0.25 nm
intervals, and eight sets of transects were selected for each, as
described above. Transects were to be flown east to west,
parallel to the long block and zone boundaries.
FIG. 2 . ThePartenavia P 68 Observerusedinthe
surveys. Note theclear
plexiglass nose, permitting unobstructedviewing of the transect centerline, and
thesidebubblewindowatthestarboardobserverstation.(Photoby
S.
Leatherwood.)
Surveys were flown at
altitudes between about 150 m and 245
m and at a ground speed of 100 knots (kts). As in our previous
aerial surveys of cetaceans (e.g., Leatherwood, 1979; Leatherwood and Reeves, 1983; Leatherwood et al., 1987), transects
were only initiated in sea surface conditions of Beaufort 3 and
below, as rougher conditions are considered to significantly
affect the probability of seeing cetaceans (e.g., Leatherwood
and Show, 1980; Scott and Gilbert, 1982:Tables 6 and 7). If
conditions deteriorated during a survey to Beaufort4 or higher
andremained so for five minutes or morethe transect was
terminated. If possible, such transects wereresumedwhen
conditions improved or were reflown on subsequent days.
Data on effort and sightings were collected from transects
(the randomly selected lines that provided the basisfor density
estimation; such periods were
logged as ‘‘on effort”) and during
transits (straight lines connecting transects with one another or
with the shoreline, routes flown alongland masses and between
the base of operations, Dutch Harbor, and starting or ending
points of transects and any survey lines completed under unacceptable conditions; such periods werelogged as “off effort”).
Data werealso recorded during the ferry flights between Anchorage and Dutch Harbor. All data were logged using an Epson
HX-20 computer linked to the aircraft navigation system
(Loran-C, Model AVA-100A, ARNAV Systems, Inc.) by
means of an RS-232 connection. Location (latitude and longitude), local time, magnetic headingand ground speed were
recorded automatically once each minute and whenever a report
of a sighting was entered. Environmental conditions, including
sea state (as Beaufort number), sun glare and characterizations
of weather and visibility, were entered periodically, as they
changed and when sightings were entered.
For each marine mammal sighting the following information
was recorded:the angle (y) formed between the horizon and a line
to the animal(s) when the aircraft was perpendicular to the
sighting (measured, to the individual or to the center of the
group of individuals, with a hand-held Suunto clinometer, and
later used to calculate perpendicular sighting distance); species;
the cue prompting the sighting; behavior; total number of
animals; swimming direction; and observer making sighting.
Once the sighting angle wasmeasured, we left the transect and
circled the animal(s) to confirm species identification, search
for calves and count individuals. The time spent circling was
considered “off effort.” Data were stored
on microcassettes and
later transferred to a WICAT computer atHubbs Marine
Research Center for analysis.
Perpendicular distance to each sighting was calculated as
X = H tan (90 - y)
(Equation 1)
where H is aircraft altitude, in feet.
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Conduct of Surveys
All surveys were flown in a Partenavia P68 Observer (Fig. 2),
a high wing, twin engine aircraft with a clear plexiglass nose
(which afforded a clear and continuous view of the transect
center line) and a 61 cm plexiglass bubble window on each side
adjacent to the observer’s seat. There were three observers. The
forward observer, seated in the Co-pilot’s position, was dedicated to observing along the transect center line. Two side
observers, who could also see the center line, searched outward
from the line. Flights were sufficiently short that rotation of
observers was unnecessary.
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36
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B.S. STEWART et a / .
Data Analysis
Density and abundance estimates were calculated using line
transect techniques (following Burnham et al., 1980) and programTRANSECT (Laake et al., 1979). Highlights of the
method as applied in thisinstance are summarized below.
The probability density function (pdf) of the perpendicular
distances, f(x), was estimated from calculated distances and
evaluated at zero (f(0)). The result was used in the following
expression for density
D = - n f(0)
(Equation 2)
2L
where n is the number of observations and L is the length, in
nautical miles, of the line(s) (i.e., the distance searched). The
value of L was calculated from recorded positions and verified
by comparison with time and speed calculations. In fact, distances calculated by the two methods differed by only three
percent.
Following Burnham etal. (1980), we selected a Fourier
series model, a linear combination of cosine functions, which
has proven generallyuseful and has been applied to a variety of
recentsurveydata (e.g., Ratti et al., 1983; Hammondand
Laake, 1983; Leatherwood et al., 1983; Leatherwood et al.,
1987). It can be expressed as
which is the product of the density of groups and an average
group size (E).
An estimate of the sampling variance for density, given by
Burnham et al. (1980), is
Var (D) = D2 (CV2(n)+ CV’(f(0)) + CV2(E))
(Equation 6)
where
CV2(n) = Var (n)/n2,
(Equation 7)
CV2(f(0)) = Var (f(O))/(f(O))’,
and
(Equation 8)
CV2(C) = var (QE2
(Equation 9)
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E-!
The variance of f(0) is from Equation 4; the variance of is the
standard sampling variance; andthe variance of n, based as it is
on replicate lines, can be expressed as
Var(n)
=
L
R- 1
R
2
4
(Equation IO)
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+
f(x) =- 1
W
x
m
ak COS ( k d W )
(Equation 3)
k= 1
where W is the half-width of the transect, in this case the largest
observed perpendicular distance, m is the number of cosine
terms used in the model, and ak is the kthparameter estimated
from the data. The estimate of f(0) is
m
+ 2
1
f(0) = W
(Equation 4)
ak
i=l
where R is the number of replicate lines, L is the total line
length, and 4 and ni are the length and number respectively of
observations for the ithreplicate.
The validity of estimates of density from line transect sampling depends on how well the following underlying assumptions are satisfied: 1) the area of interest is sampled randomly or
the population is distributed randomly within the area; 2) all
animals on or near the transect center line are seen; 3) all
measurements are made without error; 4) the animals do not
move or sampling occurs instantaneously with respect to any
movement; 5) sightings are independent events; and 6 ) the size
of a group (herd) of animals does not affect its probability of
being observed. For a detailed review of line transect theory and
methodology see Burnhamet al. (1980). For details on the use
of such techniques in censuses of cetaceans see contributors to
Chapman (1982).
k= 1
because when it is evaluated at x = 0 the cos (0) = 1.
For marine mammals that occur in groups (herds), the group
(herd), rather than the individual animal, must betreated as the
observation (Hayes, 1977;Bumham etal., 1980; Quinn, 1980).
Therefore, the number of sightings (n) is the number of groups
observed. The estimate of density, therefore, is
Z
D=- n f(0) t
(Equation 5)
2L
,
RESULTS
On flights made between 26 July and 26 August 1984 we
collected data along 3040.0 nmof survey track, including
2403.1 nm “on effort,” i.e., during random transects (Fig. 3,
top; Tables 1 and 2), and 1819.5 nm “off effort” (Fig. 3,
bottom; Tables 1 and 2). A total of about 23.6 hr was spent
searching while on transect (i.e., “on effort”), at an average
speed of 100 kts. The vast majority of effort on transect was
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TABLE 1 . Distance searched by Beaufort class
Transits
Beaufort
Areas
0-2
Blocks 1 & 2
combined
Block 3
(12.5%)
Ferry flights
Total
1284.7
(58.6%)
183.8
(87.5%)
0.0
1468.5
(61.1%)
Effort was assigned to the category
Dutch Harbor.
Transects
(on effort)
Beaufort
3-5
908.4
(41.4%)
26.2
0.0
934.6
(38.9%)
(66.4%)
(off effort)
Total
2193.1
(31.4%)
210.0
0.0
2403.1
(26.6%)
0-2
1026.6
(68.6%)
40.0
3-5
470.3
(100%)
0.0
(0%)
269.3
13.3
(95%)
(5%)
1335.9
(73.4%)
483.6
Total
Beaufort
3-5 Total
1496.9
40.0
282.6
(5%)
1819.5
0-2
2311.3
(62.6%)
223.8
(90%)
269.3
(95%)
2804.4
Total
1378.7
(37.4%)
26.2
3690.0
250.0
(10%)
13.3
282.6
1418.2
(33.6%)
4222.6
“0-2” if whitecaps were absent, “3-5” if whitecaps were present. Ferry flights are those flights between Anchorage and
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CETACEANS OFF SOUTHWESTERN ALASKA
31
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58
BERING S E A
87
56
55
5.
NORTH PACIFIC
&
‘O
83
52
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169
“
I
168
I
‘
167
I
’
166
I
I
155
I I I
I64
16s
162
1
1
161
1
1
160
I
I
t5s
I
1
158
I
I
157
I
I56
FIG.3. The distribution of transects (top) and transits (bottom). Transects were
logged as “on effort” and transits were logged as “off effort.”
spent in blocks1 and 2, where 47 of 48 planned transects were
completed. Inclement weather, mostly persistent low clouds
and fog, whichsignificantlyaffectedsurvey
conditions and
safety, permitted us to completeonly 2 of 8 transects plannedfor
block 3.
TABLE 2. Distance searched (in nautical miles) by visibility class
Transits
effort)
Visibility class
Mostly obscured <1 nm
obscured
some
Partially
1-10 nm
530.4
withUnlimited
(53.1%)
with
(32.5%)
Unlimited
(100.0%)
(10.4%)
Total
Overall, wesaw 77 groups (199 individuals) of cetaceans
(Fig. 4). The only identified baleen whale
seen on transect was a
single minke whale located off western Unalaska Island (Fig.
4). The 11 fin and 14 gray whales recorded were all seen “off
effort,” during transitor ferry flights. So also were 20 of the 26
killer whales (Orcinus orca) seen (Table 3). Only one species,
Dall’s porpoise (Phocoenoides dulli), was observed withsufficient frequency to permit estimates of density (Table 4). Three
such estimates were made: for blocks 1 and 2 combined; for
block 3; and for blocks 1, 2 and 3 combined.
There were too few
“on effort” sightings of Dall’s porpoises
to estimate f(0)reliably; so we combined “on” and “offeffort”
sightings, as described below, to derive the sightability function. Such an approach is valid if the factors affecting f(0) are
not significantly different between the sets
twoof sightings. The
factors most likelyto affect f(O), and their characterizations for
the present surveys, are:1) sea state - theproportions of
distance flown under various sea states were relatively consistent between alleffort in blocks 1 and 2 combined andeffort on
transect in block 3. Sightings from remaining flights - i.e.,
those “off effort’’ in block 3 and those during ferries - were
excluded from calculations to estimate f(0) because they were
made almost entirely in the
one category of good sea state
conditions (Table 1); 2) visibility conditions-the proportions
of distanceflownundervariousvisibility
conditions were
relatively consistent among all flights in blocks 1 and 2 combined and block 3 (Table l), so all sightings from them were
included in calculationsto estimate f(0); 3) altitude -nearly all
(91.8%) transects were flownat altitudes between about 225 m
and 245 m; therefore, sightings from “offeffort” were included
in calculations to estimate f(0) only if they were made while
flying within this range of altitudes; and
4) effects of group size
on sightability - group sizes were not substantially different
between
sightings
“on effort” (X=2.5) and sightings
“off effort” (jr = 3.8) andno differences were apparent
between the sightabilityfunctions from the twocircumstances.
Proceeding in thismanner, we were able to use 42 sightings of
Dall’s porpoises to estimate f(0).
Allof these 42 sightingsofDall’sporpoisesresultedin
recording of clinometer angle. The distribution of distances
calculated from those measured angles indicates little bias due
to rounding. This does not imply that measurements are free
from error, only that such error is random. Therefore, rather
than being grouped into distance intervals, the calculated perpendiculardistanceswere usedas exact distances to estimate f(0)
(23.0%)
1496.9
(23.5%)
Blocks 1 and 2 combined
Block
Transects
(on
(off effort)
144.9
(6.6%)
706.6
(32.2%)
(23.9%)
704.1
(32.1%)
637.543.3
(29.1%)
2193.1
129.0
(8.6%)
3
Transects
effort)
(on
0.0
(0.0%)
50.2
(35.4%)
487.0
111.5
350.5
210.0
Ferry flights
Transits
between
Anchorage
(offDutch
effort)
and
Harbor
0.0
0.0
(0.0%)
(0.0%)
29.6
(74.0%)
6.24
(15.6%)
4.16
282.6
40.0
282.6
0.0
(0.0%)
0.0
(0.08)
38
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B.S. STEWART et a1
167
162
166
163
161
167
163
I65
166
162
U
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BERING
SEA
55
BERING
SEA
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UNIYAU I.
c sowmd
A
*
54
A
4
A
r.A
&L”
A
A
YILASKA I
..
A
53
A
A
*
A
NORTH
NORTH
PACIFIC
PACIFIC
62
167
166
I65
164
163
162
161
I67
I66
165
161
163
I62
161
56
56
I1
0
A
Io
l o
59
zyxwvutsrqpo
i
zyxwvu
1,.
-
MINKE ON EFFORT
FIN OFF EFFORT
UtlD. LAFGE Wll?LE ON EFFORT
OFFEFFORT
UNID. BEAKED WHALE OFF EFFORT
OFF EFFORT
WHALE OFF EFFORT
;GRAY
HAR,pOR PORFOISE ON EFFORT
0
5s
55
BERINGSEA
I
57
U N I U I K I.
BERINGSEA
C. SOriCm.1
56
54
55
53
NORTH
PACIFIC
.
Ri
il.‘ :
54
52
53
52
Locations of sightings of cetaceaiis during transects(“on effort”) and during transits (“off effort”). The numbers by the symbols indicate the number
of
sightings at that location.
FIG. 4.
and toderive a Fourier series fit for sightings of Dall’s porpoises
(Fig. 5 ) .
Density estimates weremadeusing
the above described
estimates of f(O), the number of “on effort” sightings (n), and
in all “on effort” sightings
the average group size
(Fig. 6). We calculated an estimate for blocks 1and 2 combined
and a separate estimate for block 3 because there was considerably more effort in proportion toarea in the former than in the
latter.
To construct an overall density estimate, we weighted the
individual block estimates by the relative sizes of the areas as
D = (A1 + A2) (Dl +D2) + A3D3
(Equation 11)
Al+Az+A3
(e)
where A,, A2 andA3 are the areas (in nm) andDl, D2 and D3 are
the densities for blocks 1, 2 and 3 respectively.
DISCUSSION
The eastern North Pacific gray whale stock appears to have
recovered from the effects of the most recent episode(s) of
whaling, earlier this century, and is believed to be at or near its
pre-exploitation size of 15 000-20 000 (Reilly, 1984). The vast
majority of that population is north of Unimak Pass annually
from April-June through November-December (Jones et al.,
1984). With respect to our survey areas and times, gray whales
are peripheral, moving through UnimakPass and then eastward
close along the shores of Unimak Island and the Alaska Penin-
zyxwvutsrqponm
zyxwvutsrqpo
zyx
39
CETACEANS OFF SOUTHWESTERN ALASKA
TABLE 3. Number of sightings of marine mammals (number of individuals is shown in parentheses)
Transects (on effort)Transits
Species
Blocks
1&2 Block 3
Fin
Minke
Gray
Unid.1(1)
Killer
Unid.
Dall’s porpoise
Harbor porpoise
Total
(off effort)
BlocksBlock
1&2
3(11)
1(1)
2(2)
4(6)
Ferry Anchorage
Dutch
to
Harbor
transits)
Total
(all
3(11)
1(1)
l
4(20)
1(6)
l(1)
30(71)
2(4)
39(84)
8(26)
1(6)
16(59)
1(2)
25(93)
47(131)
4(7)
77(199)
zyxwvutsrqp
zyxwvutsrqpo
l(1)
sula during migrations. Gray whales were not takenby Akutan
whalers (Reeves et al., 1985). All of our sightings were “off
effort” and during transit along the north shore of the Alaskan
peninsula, where gray whales
were expected to beat this time of
year. We did not expect to see many in our survey area.
Minke whales of the northeastern Pacific have never been
substantiallyexploited (a few were
taken at Akutan -Reeves et
al., 1985). They are at present regarded as an Initial Management Stock (IMS) and believed to be abundant overall (IWC,
1983:97).They werethe balaenopterids seen most frequently on
recent aerial and vessel surveys in southeastern Bering Sea and
Bristol Bay (Leatherwoodet al., 1983). Their population size is
not known.
TABLE 4. Summary of statistics used in density estimates of Dall’s
porpoises and their coefficientsof variation (CV) in parentheses
A
n
f(0)
c
D
14 400
(0.209)
4 000
(0.862)
30
(0.121)
(0.450)
(0.263)
1
-
6.957
3.30
115.0
Area
Blocks 1&2
Block 3
3
whale
whale
whale
1(1)
12(21)
The pre-1905humpback whale population in the North
Pacific has been estimated as about 15 000, but the population
was subjected to extreme modem whaling through the 1960s
(Rice, 1978). Johnson and Wolman (1984) estimated the current population at about 1200, including 550-790 that winter in
Hawaiian waters(Riceand Wolman, 1984). There are data
suggestingthepopulationis
much larger.Darling
and
McSweeney (1985) estimated that there are a minimum of 1500
humpback whales inthe northeasternPacific, and Darling ( 1983)
has photoidentifiedas many as 2100 individuals in the Hawaiian
population alone. Rice (1978) reports that humpbacks, though
present in the Asian winter grounds, are now scarce in that area.
Apparently, animals from both populations occur in Alaskan
waters (Nishiwaki, 1966), but there are still only sporadic
records in the southeastern Bering Sea and along the Aleutians
et al., 1983). Humpbacks
nearUnimakPass(Leatherwood
were the second most important species to the Akutan whalers
zyxwvutsrqpo
6.957
(0.0)
1.00
-
17.0
Density (D) is expressed as numberof animals per1000 nm2;A = the size of the
areain nm; h = the number of sightings; f(0) = theprob_ailitydetection
function evaluated atzero (see text for additional details); C = the average
group (herd) size.
.5
-
;
A
m
W
;
- .3
2
I
g
.2
a
.I
-
00.C
t
zyxwv
zyxwv
‘793
)O 0.0 7
\
0.15874
0.23811
0.31740
a39685 0.47622 0.5559
P E R P E N D I C U L A R DISTANCE ( x 1
0.5
I5
( I N NAUTICAL MILES)
RG.5. Illustrationsof the fit of the Fourier series to the perpendicular distances
of
the sightings of Dall’s porpoises (f(x) = 1/W + 2.994 Cos (IT x/W) + 1.289
Cos (27rxN) and W = 0.374).
I
2
3
4
5
6
NUMBER OF ANIMALS
RG.6 . Sizes of groups (herds) of Dall’s porpoises seen during transects (“on
effort”), blocks 1, 2 and 3 combined.
40
zyxwvutsrqponm
zyxwvutsrq
zyxwvutsrq
zyxwvuts
zyxwvutsrq
B.S. STEWART et al.
numerically, constituting 30% of the total take (1510 of 5027
history of the fishery (Leatherwoodet a f . , 1985). If populations
whales identifiedto species in 23 years) but being66.7%of the
of these four species had been present
on the Akutan grounds in
total take at nearby Port Hobron
(1573 of 2357 taken identified
comparable numbers in July and August
1985, it is reasonable
to
11 years)(Reeves et af., 1985). From their
tospeciesin
suppose, from Hay's (1982) experience, thatsomewhales
apparent dispersal during recovery in various portions of the
wouldhavebeen
seen. Theappreciablenumberofsmaller
North Atlantic (IWC, 1984: 135-6),one would predict that as
animals detected suggests large numbers of whales were not
their population grows, humpbacks would recolonize former
missed simply by lack of vigilance. The results from sightings
grounds in the North Pacific.
et al.
of Dall's porpoises are a useful case in point. Leatherwood
The status oftheNorthPacificfinwhales
has notbeen
(1983) estimated that there were
97.20(SD = 49.50; CV = 0.5 1)
adequately assessed. Stocks there have remained classified by
Dall's porpoises perlo00 nm2 in study blocks between the north
theInternationalWhalingCommission(IWC)
as Protection
side of the Aleutians and about the southern
latitude of the
Stocks for a decade(Gambell, 1985) and populations were most Pribilofs, from longitude 166"W to 170"w. From the present
recently estimated to contain some 20 000 individuals, about
surveys we estimated that there were16.6 (CV = 0.0) individu38% of the pre-exploitation stock sizeof 53 OOO (Allen, 1980).
als per1000 nm2 in block3 and 115.0 (CV = 0.263) individuals
This was the species most important
to shore whalers atAkutan,
per 1OOO nm2 in blocks1 and 2 during the period of the surveys
constituting 49.7%(2498 of 5027 whales identified to species)
(Table 4). The resultsof the present surveys bracket those from
at Port
of takes there in23 years and the second most important
the previous work.
Hobron, nearly 20% (464of 2357 whales identified to species)
Results of the present surveys appear
to support the hypotheof takes there in 11 years (Reeves et al., 1985). Further, fin
sis that the relatively low numbers
of baleen whales, other than
whales were the balaenopterids seen second most often (after
gray and minke whales, seen in the
eastern Bering Sea and
minke whales) in recent surveys (Leatherwood et al., 1983).
northern North Pacific near Akutan actually
do indicate low
We expected to see them, especially on the continental shelf,
density of these animals and are not merely artifacts of sparse
during the present surveys.
coverage and poor survey conditions. However, one must be
The statusof sperm whales in the North Pacific is problematicautious when interpreting a scarcity of sightings of cetaceans
cal and highly disputed. For the present, the species there is
from aerial surveys as evidence of theirlow density inthe
managed in two divisions, eastern and western (Gosho et al.,
area(s) under study, unless survey methods have been carefully
1984), which are at reducedlevels. There apparently are 61 OOO
controlled to maximize the probability of sightings. Such was
males over 10 years of age in the western North Pacific and
the case. First, present surveys used anaircraft with downward
11 1 400 over 12 years of age in the eastern North
Pacific, 47%
visibility, permitting observersto see the transect
center line and
and 79% oftheoriginal(in
1910) stocksizesrespectively
thereby more nearly satisfying the second assumption of line(Gosho et al., 1984:Table 4). Whatever the correct delineations
transect methodology(i.e., that all animalson or near the track
of stocks and actual numbers, adult males from theeastern and
line are seen). Such increased visibility would result in larger
western Pacific intermingle(d) in higher
latitudes, and we would numbers of sightings near the center
line. The absence of data in
not have been surprisedto have encountered a few malesperm
that strip couldsignificantlyaffectcredibility
of estimates.
whales in the deeper water portions of the surveyareas.
There were few sightings of cetaceans during our surveys, but
The other three northern North Pacific great whales are not
whenallsightings(includingpinnipedsandsea
otters, not
commonly reported inor near any of the three study blocks and analyzed) werecombined, about 25%of them(51 of 206) were
so were not expectedon these surveys. Bowheads may assemble within 0.04 nm of the transect center line.
Second, present surveys were conducted only in acceptable
et al., 1980;
near St. MatthewIslandinspring(Braham
conditions of sea state and visibility (91%of the survey effort
Brueggeman et af., 1984) but are rarely reported farther south
(Leatherwood et af., 1983); right whales are seriously endanwas in Beaufort 3 or below, 61% inthetwobestvisibility
gered and rarely seen anywhere in the eastern North Pacific
classes), when the probability of detecting animals is highest.
(Rice, 1974; Brownell et al., 1986; Scarff, 1986; Reeves and
This was made possible by the proximitylines
of in blocks1 and
Leatherwood, 1985); and sei whales are generally uncommon
2 to the operational base and the relatively short time required to
north of the Aleutians, being found in pelagic regions farther
complete a replicate setof transects ineach. Therefore, observsouth (Rice, 1974:181;Leatherwood et al., 1983).
ers were afforded the luxuryof waiting at the operational base
With the above mind,
in there were surprisingly
few sightings
for acceptable weather conditions before departing for survey
of great whales in or near the rou hly14 400 nm2 area of study
and of surveyingon whichever side of the Aleutiansoffered the
blocks 1 and 2 or in the 4000 nm!?
area of block 3 during the 29
best weather conditions. The absence of anylee effect at block
field days. By comparison, in surveys byaircraft of portions of
3, the greater distance to that block and the often significant
an approximately 50 000 nm2 area within about100 nm ofshore
differencesinweathernearthe
chain andweather offshore
off eastern Newfoundland-Labrador in August
1980, Hay (1982)
(making difficult any decisions of when conditions would be
observed 3 1 groups of humpback whales and 18 groups of fin
3) resulted in completion of only
acceptable for surveying block
whales,supporting his estimatesofpopulations
of 738
one of four planned replicates in block 3 in 29 possible survey
(SD = 221) and 478 (SD = 250) forthe two species respectively.
days. Previous surveys ofthe Bering Sea (Leatherwood et af.,
1983) hadcovered large areas, includingmany for which
Hay's surveys were designed to cover essentially the whaling
accurate weather reporting is not available. The
result was a
groundsusedbyCanadianwhalersfrom
SouthDildo and
high percentageof time in conditions
of unacceptable visibility.
1964 through 1971
Williamsport,Newfoundland,between
Third, the eight sets of replicates in blocks 1 and 2 were
(Mitchell, 1974:Fig.5-1). From cumulativecatches, it has been
completed within amonth, at a timeof year when peakcatches
estimated there were populations of at least 1500 fin, lo00
of fin, humpback,blue and sperm whales were made (Leatherhumpback, 500 blue and 300 sperm whales available within a
100 nm radius of the Akutan whaling station at some point
the inwood et af., 1985). Further, transects were spaced at narrow
zyxwvutsrqp
zyxwvutsr
CETACEANS OFF SOUTHWESTERN ALASKA
41
of density from line transect sampling of biological populations. Wildlife
distance intervals, affording higher coverage (per survey and
overall, during the month) with concomitant higher probability Monographs 72. 202 p.
CHAPMAN, D.G., chairman. 1982. Report of the workshop on the design of
of detecting animals present than on previous surveys of the
sightings surveys.Reports of theInternationalWhalingCommission
area.
32531-549.
DARLING, J.D. 1983. Migrations,abundance, and behavior of Hawaiian
Fourth, special attention was paid to precision in distance
humpbackwhales Megapfera novaeangliae. Ph.D. thesis, University of
estimation (helped by the increase in proportion of sightings
California,
Santa CNZ, California. AM Arbor,Michigan,University
close to the aircraft wherean error of afew degrees amounts to
Microfilms. 147 p.
an error <0.004 nm in the estimated perpendicular sighting
-and McSWEENEY,D.J. 1985. Observations on themigrations of
distance) and to remaining with groups
long enough to confirm
North Pacific humpback whales(Megapferanovaeangliae). Canadian Journal of Zoology 63:308-314.
speciesandnumberofindividualspresent.
The addedtime
GAMBELL, R. 1985. Fin whaleBalaenopreraphysalus (Linnaeus, 1758). In:
required for these last activities is notavailable on longer
Ridgway, S.H., and Harrison, R., eds. Handbook of Marine Mammals.
surveys, in which the aircraft
is stretched to safety limitsjust to
Volume 3: The Sireniansand Baleen Whales. 171-192.
complete transects.
GOSHO, M.E., RICE, D.W., and BRIEWICK, J.M. 1984. The sperm whale,
One problemthatwillalways
exist inaerialsurveysof
Physefer macrocephalus.Marine Fisheries Review46(4):54-64.
cetaceansisthatofestimatingnumbersofanimalsmissed
HAMMOND, P.S., and LAAKE,J.L. 1983. Trends in estimates of abundance
because they were submerged, and therefore not visible, during of dolphins (Sfenellaspp. and Delphinus delphis) involved in the purse-seine
fishery for tunas in the eastern Pacific Ocean, 1977-1981. Reports of the
et al., 1982). This
the period of the overflight (Leatherwood
International Whaling Commission33565-588.
problem can only be corrected meaningfully withdata, preferHAY, K. 1982. Aerial line-transect estimatesof abundance of humpback, fin
ably collected at the time of the surveys,on diving frequencies
and long-finned pilot whales in the Newfoundland-Labrador area. Reports
of
the International Whaling Commission32:475-489.
and times for each species seen and their resultant effects on
HAYES, R. 1977. A critical review of line transect methods. M.S. thesis,
visibility. Submergence is likely a more significant problemin
University of Edinburgh, Scotland.
attempts to estimate density of great whales (which usually
INTERNATIONALWHALINGCOMMISSION (IWC). 1983. Thirty-third
travel singly or in small groups and remain submerged
for long
report of theInternational Whaling Commission. Reports
of the International
periods), particularly when they
occur in low densities, thanit is
Whaling Commission 33. 782 p.
-.
1984. Thirty-fourth reportof the International Whaling Commission.
with animals such as Dall’s porpoises, which travel in larger
Reports of the International Whaling Commission34. 752 p.
groups and remain submergedfor shorter periods.
zyxwvutsrqp
zyxwvutsrq
zyxwvut
zyx
JOHNSON, J.H., and WOLMAN, A.E. 1984. The humpback whale,Megaptera novaeangliae. Marine Fisheries Review46(4):30-37.
JONES, M.L., SWARTZ, S.L., and LEATHERWOOD, S . , eds. 1984. The
ACKNOWLEDGEMENTS
Gray Whale. Orlando, Florida: AcademicPress. 600 p.
LAAKE, J.L., BURNHAM, K.P., andANDERSEN, D.R. 1979. Users
We thank the following:J.D. Hall provided generous assistance and
manual for Program TRANSECT. Logan, Utah: Utah State University Press.
support throughout the surveys;
S . and T. Madsen (Aleutian Air, Ltd.)
26 p.
radioedweatherreports to us fromDutchHarborwhilewewere
LEATHERWOOD, S . 1979. Aerial surveyof the bottlenosedolphin, Tursiops
conducting surveys offshore;K. Springer (Chevron Oil Corp.) allowed truncafus,and the West Indian Manatee,Trichechus manarus,in the Indian
us access to SEDCO oil rig radio frequencies and MERISTAT Num77:47-59.
and Banana Rivers, Florida. United States Fishery Bulletin
REEVES, R.R. 1983. Abundanceof bottlenose dolphins in Corpus
R. Landenberger (NORTEC) -and
bers to obtain weather reports from them;
communicated weather conditions us;
to and employees at Air Pac and Christi Bay and coastal southern Texas. Contributions to Marine Science
26179-199.
ReeveAirandresidentsofthe
town of DutchHarborgavetheir
S., and SHOW, I.T., Jr. 1980. Developmentof systematic
assistance duringour stay at Unalaska Island. The Partenavia P68 was LEATHERWOOD,
procedures for estimating size
of “population(s)” of bottlenose dolphinsand
owned by Dr. R. and Mr. W. Sutherland and was flown byD. Warth.
estimates of sizes of “population(s)” of bottlenose dolphins in three geoS . Ingram and C. Hayashi prepared the figures. E. Garner typed the
graphical areas; with incidental observations of West Indian manatees and
manuscript. The project was sponsored by NOAA, National Ocean
marine turtles. Final Report on contract NA-79-GAC-0038. Submitted to
Service, Mr. L. Jarvella, Contract No. NA82RAC00039.
U.S. Department of Commerce, NOAA, NMFS, Miami, Florida. 98 p.
LEATHERWOOD, S . , BOWLES, A.E., and REEVES, R.R. 1983. Aerial
Surveys of marine mammals in the southeastern BeringSea. U.S. Department of Commerce, NOAA, OCSEAP, Final Report.42(1986):147-490.
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