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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">tinro</journal-id><journal-title-group><journal-title xml:lang="ru">Известия ТИНРО</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya TINRO</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1606-9919</issn><issn pub-type="epub">2658-5510</issn><publisher><publisher-name>ТИНРО</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.26428/1606-9919-2022-202-187-207</article-id><article-id custom-type="elpub" pub-id-type="custom">tinro-711</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>УСЛОВИЯ ОБИТАНИЯ ПРОМЫСЛОВЫХ ОБЪЕКТОВ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ENVIRONMENTS OF FISHERIES RESOURCES</subject></subj-group></article-categories><title-group><article-title>Многолетние изменения термических условий на поверхности дальневосточных морей и СЗТО и их связь с крупномасштабными климатическими процессами</article-title><trans-title-group xml:lang="en"><trans-title>Long-term changes in thermal conditions on the surface of the Far-Eastern Seas and North-West Pacific and their relationship with large-scale climate processes</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-3966-6208</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хен</surname><given-names>Г. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Khen</surname><given-names>G. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Хен Геннадий Васильевич, кандидат географических наук, ведущий научный сотрудник</p><p>690091, г. Владивосток, пер. Шевченко, 4</p></bio><bio xml:lang="en"><p>Gennady V. Khen, Ph.D., leading researcher</p><p>4, Shevchenko Alley, Vladivostok, 690091, Russia</p></bio><email xlink:type="simple">gennady.khen@tinro-center.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2322-8505</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Устинова</surname><given-names>Е. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Ustinova</surname><given-names>E. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Устинова Елена Ивановна, кандидат географических наук, ведущий научный сотрудник</p><p>690091, г. Владивосток, пер. Шевченко, 4</p></bio><bio xml:lang="en"><p>Elena I. Ustinova, Ph.D., leading researcher</p><p>4, Shevchenko Alley, Vladivostok, 690091, Russia</p></bio><email xlink:type="simple">elena.ustinova@tinro-center.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Сорокин</surname><given-names>Ю. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Sorokin</surname><given-names>Yu. D.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Сорокин Юрий Дмитриевич, ведущий специалист</p><p>690091, г. Владивосток, пер. Шевченко, 4</p></bio><bio xml:lang="en"><p>Yuriy D. Sorokin, leading specialist</p><p>4, Shevchenko Alley, Vladivostok, 690091, Russia</p></bio><email xlink:type="simple">yuriy.sorokin@tinro-center.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Тихоокеанский филиал ВНИРО (ТИНРО)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Pacific branch of VNIRO (TINRO)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>09</day><month>04</month><year>2022</year></pub-date><volume>202</volume><issue>1</issue><fpage>187</fpage><lpage>207</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хен Г.В., Устинова Е.И., Сорокин Ю.Д., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Хен Г.В., Устинова Е.И., Сорокин Ю.Д.</copyright-holder><copyright-holder xml:lang="en">Khen G.V., Ustinova E.I., Sorokin Y.D.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://izvestiya.tinro-center.ru/jour/article/view/711">https://izvestiya.tinro-center.ru/jour/article/view/711</self-uri><abstract><p>Исследованы закономерности многолетних изменений температуры поверхности океана (ТПО) в дальневосточных морях и северо-западной части Тихого океана (СЗТО) в 1950–2019 гг. Во все сезоны года температура воды повышалась, при этом зимой и осенью тренды выражены наиболее ярко, а летом они менее показательны. Проведен анализ связей между ТПО трех дальневосточных морей России и СЗТО и 8 основными для северной части Тихого океана климатическими индексами: AO, Nino 3.4, PDO, ALPI, NPI, PNA, SHI, WP. В Беринговом море резкий скачок ТПО произошел в 1977 г., он совпал с резким изменением во временном ходе индексов PDO, ALPI, NPI и PNA. В Охотском море такой скачок пришелся на 1981 г., в Японском море — на 1990 г., через год после резких перепадов в ходе АО, PDO и PNA. В 2008 и 2018 гг. наблюдались небольшие скачки температуры в СЗТО. Основной вклад в изменчивость температуры Берингова моря во все сезоны вносит PDO. Зимой и весной заметную роль играют ALPI и PNA. Для Охотского моря основное значение имеет АО, для Японского — AO, SHI и WP. В СЗТО во все сезоны значимые связи между ТПО и индексами не наблюдаются. По вкладу в изменчивость ТПО в отдельных районах дальневосточного бассейна индексы можно разделить на две категории: западные и восточные. К первой относятся АО, SHI и WP, которые воздействуют на западную часть бассейна, условно ограниченную долготой Камчатки. К основным индексам восточной части относятся PDO, PNA и ALPI.</p></abstract><trans-abstract xml:lang="en"><p>Previously published results of the study [Khen et al., 2019b] are continued. Long-term changes of the sea surface temperature (SST) in the Far-Eastern Seas and North-West Pacific (NWP) are described for 1950–2019 and their relationship with large-scale climate processes described by climatic indices (AO, Nino 3.4, PDO, ALPI, NPI, PNA, SHI, and WP) is analyzed. SST has increased in all seasons, with higher rate in winter and autumn and less significant trend in summer. A prominent shift to warmer regime occurred in the Bering Sea in 1977 that coincided with a sharp change in dynamics of PDO, ALPI, NPI, and PNA indices. Such shifts were observed in the Okhotsk Sea in 1981 and in the Japan Sea in 1990, one year after the shifts in the time-series of AO, PDO, and PNA indices. Smaller shifts to warming happened in NWP in 2008 and 2018. Pacific Decadal Oscillation is the main contributor to temperature variability in the Bering Sea in all seasons, though the contribution of ALPI and PNA variation is considerable in winter and spring. Arctic Oscillation is the most important for the Okhotsk Sea. Variations of AO, SHI and WP are significant for the SST variability in the Japan Sea. Any single climatic index does not determine the SST variability in NWP, in all seasons. The set of climatic indices can be divided into two categories: western and eastern ones, according to their contribution to SST variability in certain regions. The western group includes AO, SHI, and WP, which contribute mostly to the variations in the western regions, westward from the longitude of Kamchatka. The most important indices in the eastern group are PDO, PNA and ALPI.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>дальневосточные моря России</kwd><kwd>СЗТО</kwd><kwd>климатические индексы</kwd><kwd>ТПО</kwd><kwd>климатические сдвиги</kwd><kwd>связи</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Far-Eastern Seas</kwd><kwd>North-West Pacific</kwd><kwd>climate index</kwd><kwd>SST</kwd><kwd>climate shift</kwd><kwd>atmosphere-ocean relationship</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Результаты настоящего исследования были получены в рамках выполнения государственного задания № 076-00005-20-00 ФГБНУ «ВНИРО» на 2020 г.</funding-statement><funding-statement xml:lang="en">Results of this study were obtained within implementation of the government assignment No. 076-00005-20-00 to the Federal State Budgetary Research Institution VNIRO for 2020</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Басюк Е.О., Зуенко Ю.И. 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