Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences

Recently the sea ice edge at Chukotka retreats further northward in summer and new ice formation begins in a month later in autumn than in previous decades because of climate change that changes the pacific walrus Odobenus rosmarus divergens habitat. Now the Bering Sea becomes completely clear of th...

Full description

Bibliographic Details
Main Authors: Sergey V. Zagrebelny, Anatoly A. Kochnev
Format: Article
Language:Russian
Published: Transactions of the Pacific Research Institute of Fisheries and Oceanography 2017-09-01
Series:Известия ТИНРО
Subjects:
Online Access:https://izvestiya.tinro-center.ru/jour/article/view/316
_version_ 1797696623221932032
author Sergey V. Zagrebelny
Anatoly A. Kochnev
author_facet Sergey V. Zagrebelny
Anatoly A. Kochnev
author_sort Sergey V. Zagrebelny
collection DOAJ
description Recently the sea ice edge at Chukotka retreats further northward in summer and new ice formation begins in a month later in autumn than in previous decades because of climate change that changes the pacific walrus Odobenus rosmarus divergens habitat. Now the Bering Sea becomes completely clear of the ice by start of the spring migration of walruses. In these conditions, the walrus migration routes and feeding grounds location changes. Permanent walrus rookeries on the eastern coast of Chukotka and Kamchatka disappeared (Verkhoturov Island, Karaginsky Island, Bogoslov Islands, Anastasia Bay, Cape Dezhnev, Cape Sery, Cape Olutorsky, Cape Zosima) and new rookeries have formed in the Bering Sea (at Meinypylgino and Enmelen) and on the Arctic shore of Chukotka (at Vankaren and Cape Shmidt). Benthos community has changed, too. As the result, quality of the walrus habitat became worse, the sickness and mortality of young animals increased and the reproduction rate decreased. Formerly stable large walrus rookery in the Krest Bay (Meeskyn) was surveyed in 2016. Together with Retkyn rookery in the Rudder Bay it formed the large Anadyr group of walruses, about 50,000 of the animals gathered on these rookeries in the 1980s. However, the group began to fluctuate with decreasing trend since the 1990s: its number was estimated as 5,000-6,000 animals in 1996, 12,000 in 1997, 30,000 in 1999, 26,000 in 2000, 6,000-8,000 in 2001-2007, 2,000 in 2008. Meeskyn rookery did not function since 2006, though small group of 200 animals was observed here in 2016. Two hypotheses on this tendency are proposed: i) negative influence of climate change on reproduction of walruses in the Chukchi Sea; ii) depletion of the walrus feeding grounds in the Anadyr Bay caused by climate change and excessive abundance of the population.
first_indexed 2024-03-12T03:29:04Z
format Article
id doaj.art-8cd835ed9179420ca800958f90aa12a0
institution Directory Open Access Journal
issn 1606-9919
2658-5510
language Russian
last_indexed 2024-03-12T03:29:04Z
publishDate 2017-09-01
publisher Transactions of the Pacific Research Institute of Fisheries and Oceanography
record_format Article
series Известия ТИНРО
spelling doaj.art-8cd835ed9179420ca800958f90aa12a02023-09-03T13:29:21ZrusTransactions of the Pacific Research Institute of Fisheries and OceanographyИзвестия ТИНРО1606-99192658-55102017-09-011903627110.26428/1606-9919-2017-190-102-111314Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequencesSergey V. Zagrebelny0Anatoly A. Kochnev1ЧукотНИО Тихоокеанского научно-исследовательского рыбохозяйственного центраИнститут биологических проблем Севера ДВО РАН; Национальный парк «Берингия»Recently the sea ice edge at Chukotka retreats further northward in summer and new ice formation begins in a month later in autumn than in previous decades because of climate change that changes the pacific walrus Odobenus rosmarus divergens habitat. Now the Bering Sea becomes completely clear of the ice by start of the spring migration of walruses. In these conditions, the walrus migration routes and feeding grounds location changes. Permanent walrus rookeries on the eastern coast of Chukotka and Kamchatka disappeared (Verkhoturov Island, Karaginsky Island, Bogoslov Islands, Anastasia Bay, Cape Dezhnev, Cape Sery, Cape Olutorsky, Cape Zosima) and new rookeries have formed in the Bering Sea (at Meinypylgino and Enmelen) and on the Arctic shore of Chukotka (at Vankaren and Cape Shmidt). Benthos community has changed, too. As the result, quality of the walrus habitat became worse, the sickness and mortality of young animals increased and the reproduction rate decreased. Formerly stable large walrus rookery in the Krest Bay (Meeskyn) was surveyed in 2016. Together with Retkyn rookery in the Rudder Bay it formed the large Anadyr group of walruses, about 50,000 of the animals gathered on these rookeries in the 1980s. However, the group began to fluctuate with decreasing trend since the 1990s: its number was estimated as 5,000-6,000 animals in 1996, 12,000 in 1997, 30,000 in 1999, 26,000 in 2000, 6,000-8,000 in 2001-2007, 2,000 in 2008. Meeskyn rookery did not function since 2006, though small group of 200 animals was observed here in 2016. Two hypotheses on this tendency are proposed: i) negative influence of climate change on reproduction of walruses in the Chukchi Sea; ii) depletion of the walrus feeding grounds in the Anadyr Bay caused by climate change and excessive abundance of the population.https://izvestiya.tinro-center.ru/jour/article/view/316тихоокеанский моржodobenus rosmarus divergensраспределениебереговые лежбищамиграционная активностьанадырский заливчукоткакамчаткаpacific walrusodobenus rosmarus divergenswalruses distributioncoastal rookerywalruses migrationanadyr baychukotkakamchatka peninsula
spellingShingle Sergey V. Zagrebelny
Anatoly A. Kochnev
Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
Известия ТИНРО
тихоокеанский морж
odobenus rosmarus divergens
распределение
береговые лежбища
миграционная активность
анадырский залив
чукотка
камчатка
pacific walrus
odobenus rosmarus divergens
walruses distribution
coastal rookery
walruses migration
anadyr bay
chukotka
kamchatka peninsula
title Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
title_full Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
title_fullStr Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
title_full_unstemmed Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
title_short Influence of climate change on summer-fall distribution of pacific walrus in the western Bering Sea: analysis of reasons and consequences
title_sort influence of climate change on summer fall distribution of pacific walrus in the western bering sea analysis of reasons and consequences
topic тихоокеанский морж
odobenus rosmarus divergens
распределение
береговые лежбища
миграционная активность
анадырский залив
чукотка
камчатка
pacific walrus
odobenus rosmarus divergens
walruses distribution
coastal rookery
walruses migration
anadyr bay
chukotka
kamchatka peninsula
url https://izvestiya.tinro-center.ru/jour/article/view/316
work_keys_str_mv AT sergeyvzagrebelny influenceofclimatechangeonsummerfalldistributionofpacificwalrusinthewesternberingseaanalysisofreasonsandconsequences
AT anatolyakochnev influenceofclimatechangeonsummerfalldistributionofpacificwalrusinthewesternberingseaanalysisofreasonsandconsequences