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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">10.26428/1606-9919-2020-200-58-81</article-id><article-id custom-type="elpub" pub-id-type="custom">tinro-538</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>БИОЛОГИЧЕСКИЕ РЕСУРСЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>BIOLOGICAL RESOURCES</subject></subj-group></article-categories><title-group><article-title>СВЯЗЬ ЗАПАСОВ ЧЕРНОГО ПАЛТУСА В ОХОТСКОМ МОРЕ С ФАКТОРАМИ ВНЕШНЕЙ СРЕДЫ</article-title><trans-title-group xml:lang="en"><trans-title>RELATIONSHIP OF THE GREENLAND HALIBUT STOCKS IN THE OKHOTSK SEA WITH ENVIRONMENTAL FACTORS</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кулик</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kulik</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кулик Владимир Владимирович, кандидат биологических наук, начальник отдела</p></bio><bio xml:lang="en"><p>Kulik Vladimir V., Ph.D., head of department</p><p>4, Shevchenko Alley, Vladivostok, 690091</p></bio><email xlink:type="simple">vladimir.kulik@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>Пранц</surname><given-names>C. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Prants</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Пранц Сергей Владимирович, доктор физико-математических наук, профессор, заведующий лабораторией</p></bio><bio xml:lang="en"><p>Prants Sergey V., D.Phys., professor, head of laboratory</p><p>43, Baltiyskaya Str., Vladivostok, 690041</p></bio><email xlink:type="simple">prants@poi.dvo.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Будянский</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Budyansky</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Будянский Максим Васильевич, кандидат физико-математических наук, старший научный сотрудник</p></bio><bio xml:lang="en"><p>Budyansky Maxim V., Ph.D., senior researcher</p><p>43, Baltiyskaya Str., Vladivostok, 690041</p></bio><email xlink:type="simple">plaztic@poi.dvo.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Улейский</surname><given-names>М. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Uleysky</surname><given-names>M. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Улейский Михаил Юрьевич, кандидат физико-математических наук, ведущий научный сотрудник</p></bio><bio xml:lang="en"><p>Uleysky Mikhail Yu., Ph.D., leading researcher</p><p>43, Baltiyskaya Str., Vladivostok, 690041</p></bio><email xlink:type="simple">uleysky@poi.dvo.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Файман</surname><given-names>П. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Fayman</surname><given-names>P. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Файман Павел Аркадьевич, кандидат физико-математических наук, старший научный сотрудник</p></bio><bio xml:lang="en"><p>Fayman Pavel A., Ph.D., senior researcher</p><p>43, Baltiyskaya Str., Vladivostok, 690041</p></bio><email xlink:type="simple">pfayman@poi.dvo.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Глебов</surname><given-names>И. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Glebov</surname><given-names>I. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Глебов Игорь Иванович, кандидат биологических наук, заведующий лабораторией</p></bio><bio xml:lang="en"><p>Glebov Igor I., Ph.D., head of laboratory</p><p>4, Shevchenko Alley, Vladivostok, 690091</p></bio><email xlink:type="simple">igor.glebov@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>Глебова</surname><given-names>С. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Glebova</surname><given-names>S. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Глебова Светлана Юрьевна, кандидат географических наук, ведущий научный сотрудник</p></bio><bio xml:lang="en"><p>Glebova Svetlana Yu., Ph.D., leading researcher</p><p>4, Shevchenko Alley, Vladivostok, 690091 </p></bio><email xlink:type="simple">svetlana.glebova@tinrocenter.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>Новиков</surname><given-names>Р. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Novikov</surname><given-names>R. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Новиков Роман Николаевич, старший научный сотрудник</p></bio><bio xml:lang="en"><p>Novikov Roman N., senior researcher</p><p>18, Naberezhnaya Str., Petropavlovsk-Kamchatsky, 683000</p></bio><email xlink:type="simple">novikov.r.n@kamniro.ru</email><xref ref-type="aff" rid="aff-3"/></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><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Тихоокеанский океанологический институт им. В.И. Ильичева ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Pacific Oceanological Institute, Far East Branch, Russian Ac. Sci.</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Камчатский филиал ВНИРО (КамчатНИРО)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kamchatka branch of VNIRO (KamchatNIRO)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>30</day><month>03</month><year>2020</year></pub-date><volume>200</volume><issue>1</issue><fpage>58</fpage><lpage>81</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кулик В.В., Пранц C.В., Будянский М.В., Улейский М.Ю., Файман П.А., Глебов И.И., Глебова С.Ю., Новиков Р.Н., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Кулик В.В., Пранц C.В., Будянский М.В., Улейский М.Ю., Файман П.А., Глебов И.И., Глебова С.Ю., Новиков Р.Н.</copyright-holder><copyright-holder xml:lang="en">Kulik V.V., Prants S.V., Budyansky M.V., Uleysky M.Y., Fayman P.A., Glebov I.I., Glebova S.Y., Novikov R.N.</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/538">https://izvestiya.tinro-center.ru/jour/article/view/538</self-uri><abstract><p>Представлена оценка динамики биомассы черного палтуса в различных подзонах промысловой зоны Охотское море. Обнаружена значимая (p &lt; 0,05) отрицательная корреляция изменений промыслового запаса (FSB) в подзоне Восточно-Сахалинской (ПВС) с численностью трехгодовиков в остальных подзонах Охотского моря с учетом необходимых временных сдвигов в 3 года (r = –0,53) и в 4 года (r = –0,49). Эта численность, в свою очередь, значимо и положительно связана (r = 0,52, p &lt; 0,05) с изменениями индексов зонального переноса в январе и меридионального в марте, произошедшими в год рождения пополнения. Ошибки определения зависимости величины этого пополнения от нерестового запаса по зависимости Бивертона-Холта значимо положительно (r = 0,64, p = 0,03) связаны с индексом арктического колебания. Циркуляция в Охотском море названа прямой причиной сноса икры, личинок и молоди черного палтуса с нерестилищ в восточной части моря в западную. Перенос будущего пополнения черного палтуса моделировался адвекцией искусственных пассивных частиц в поле скорости численной модели циркуляции JCOPE2. Использованы гидрофизические поля для Охотского моря с 1993 по 2017 г. в слое 40–50 м, где предполагается основной перенос икры, личинок и молоди. Пассивные частицы (250 тыс. шт.), имитирующие икру и личинок рыб, запускались у западной Камчатки в районе с максимальной концентрацией преднерестовых и нерестовых самок черного палтуса. Рассчитывалась доля частиц, дошедших до выделенных разрезов у восточного Сахалина, а также пути их переноса и распределение по времени прибытия на эти разрезы. Обнаружена значимая положительная корреляция (r = 0,44, p &lt; 0,05) доли частиц, запущенных в декабре и дошедших до северного разреза у восточного Сахалина менее чем за 150 дней, с изменениями FSB через 6 лет в ПВС. Еще более высокая корреляция (r = 0,94, p &lt; 0,05) обнаружена c FSB в ПВС при запуске частиц в октябре и ноябре при учете их нелинейного оптимума в обобщенной аддитивной модели. Таким образом, показан механизм прямого влияния циркуляции на FSB в ПВС путем переноса части будущего пополнения из восточной части моря. В итоге сделан прогноз о снижении FSB в ПВС в ближайшие 6 лет.</p><p>Авторы заявляют, что настоящая работа не содержит собственных экспериментальных данных, полученных с использованием животных или с участием людей. Библиографические ссылки на все использованные данные других авторов оформлены в соответствии с ГОСТом.</p><p>Авторы заявляют, что у них нет конфликта интересов.</p></abstract><trans-abstract xml:lang="en"><p>Dynamics of the greenland halibut biomass in the fishery districts of the Okhotsk Sea (or subzones) is considered. The biomass variation in the East-Sakhalin subzone has a significant (p &lt; 0.05) negative correlation with the number of 3+ fish in other subzones, with the time lag of 3 years (r = –0.53) and 4 years (r = –0.49), that is interpreted as alternative distribution of the halibut recruitment from the common spawning area either to this district or other ones. From other hand, the recruits abundance in other districts is significantly and positively associated (r = 0.52, p &lt; 0.05) with the index of zonal atmosphere transfer in January and with the index of meridional atmosphere transfer in March of the years of hatching. The recruitment dependence on the spawning stock could be explained by Beaverton-Holt equation with the residuals significantly and positively (r = 0.64, p = 0.03) related with the Arctic Oscillation index. Transport of the eggs, larvae and juveniles of greenland halibut from the spawning grounds at western Kamchatka to the western Okhotsk Sea is considered as the mechanism of its recruitment distribution between the districts in relation with atmospheric indices. The transport was simulated for 1993–2017 using the circulation model JCOPE2 as the movement of 250,000 artificial passive particles, imitating eggs and larvae, with water flows at the depth 40–50 m where their main aggregations are supposed. The particles were released in the area at western Kamchatka where the maximal concentration of spawning females occurred. Number of the particles reached the sections off eastern Sakhalin and their arrival times were computed, their pathways were tracked. The portion of particles released in December and reached northern Sakhalin within 150 days changed in significant positive correlation (r = 0.44, p &lt; 0.05) with dynamics of the halibut stock in the East-Sakhalin subzone, with the time lag 6 years. Even closer correlation (r = 0.94, p &lt; 0.05) could be found for the optimum income of the particles released in October or November in the general additive model of the stock. Using the model results for the recent years, the greenland halibut stock decreasing in the East-Sakhalin subzone is forecasted for the next 6 years.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>черный палтус</kwd><kwd>вылов</kwd><kwd>Охотское море</kwd><kwd>циркуляция</kwd><kwd>адвекция пассивных частиц</kwd></kwd-group><kwd-group xml:lang="en"><kwd>greenland halibut</kwd><kwd>fishery</kwd><kwd>Okhotsk Sea</kwd><kwd>water circulation</kwd><kwd>transport of eggs and larvae</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа С.В. Пранца, М.В. Будянского, М.Ю. Улейского и П.А. Файмана по лагранжеву моделированию финансово поддержана Российским научным фондом в рамках проекта № 19-17-00006. Оценка состояния запасов черного палтуса проведена в рамках государственного задания № 076-00005-19-00 ФГБНУ «ВНИРО» на 2019 г. Авторы выражают признательность всем участникам научных рейсов и наблюдателям на промысле, чьи материалы использованы для настройки модели «Синтез», а также руководству Центра системы мониторинга рыболовства и связи за предоставление доступа к Отраслевой системе мониторинга для получения судовых суточных наблюдений. Благодарим сотрудников JAMSTEC за проведение эксперимента JCOPE2. Особая благодарность авторам моделей «Синтез» О.И. 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