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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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.7868/S2073667321040055</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-132</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>ГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>HYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSES</subject></subj-group></article-categories><title-group><article-title>Пространственно-временные характеристики апвеллингов в Юго-Восточной Балтике в 2010–2019 гг.</article-title><trans-title-group xml:lang="en"><trans-title>Upwelling spatiotemporal characteristics in the southeastern Baltic Sea in 2010–2019</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>Капустина</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kapustina</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Нахимовский пр., д. 36, г. Москва</p></bio><bio xml:lang="en"><p>117997, Nahimovskiy prospekt, 36, Moscow</p></bio><email xlink:type="simple">kapustina.mariya@ya.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>Зимин</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Zimin</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Нахимовский пр., д. 36, г. Москва</p><p>199034, Университетская наб., 7–9, г. Санкт-Петербург</p></bio><bio xml:lang="en"><p>117997, Nahimovskiy prospekt, 36, Moscow</p><p>199034, 7–9, Universitetskaya Nab., St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН; Санкт-Петербургский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences; St. Petersburg State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>14</day><month>12</month><year>2021</year></pub-date><volume>14</volume><issue>4</issue><fpage>52</fpage><lpage>63</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Капустина М.В., Зимин А.В., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Капустина М.В., Зимин А.В.</copyright-holder><copyright-holder xml:lang="en">Kapustina M.V., Zimin A.V.</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://hydrophysics.spbrc.ru/jour/article/view/132">https://hydrophysics.spbrc.ru/jour/article/view/132</self-uri><abstract><p>В работе представлены результаты верификации и применения предложенного автоматического алгоритма определения апвеллинга по данным реанализа CMEMS Baltic Sea Physical Reanalysis product в юго-восточной части Балтийского моря за 2010–2019 гг. Верификация работы алгоритма выполнена по данным многомесячных наблюдений на морской ледостойкой стационарной платформе D6, судовым данным, полученным в 127-м рейсе НИС «Профессор Штокман» в 2014 г., и результатам выделения апвеллинга по температуре поверхности моря по данным спектрорадиометра MODIS Terra/Aqua. Показано, что наименьшая повторяемость апвеллингов наблюдается в августе-сентябре (5–6 дней в год), наибольшая — в мае — июне и октябре (11–15 дней в год). В период 2010–2013 гг. в исследуемом районе наблюдалось в среднем до 10 % отрицательных термических аномалий в теплый период года. С 2014 г. (за исключением 2017 г.) отмечено увеличение повторяемости апвеллингов — в среднем, около 20 % дней составляли дни с апвеллингом. Показано, что зимние индексы колебания Восточная Атлантика — Западная Россия, восточно-атлантического колебания и весенний индекс скандинавского колебания могут быть использованы для оценок характеристик будущего летнего апвеллинга.</p></abstract><trans-abstract xml:lang="en"><p>The article presents the results of verification and application of the proposed automatic algorithm of upwelling detection and presents the results of its work based on the CMEMS Baltic Sea Physical Reanalysis product in the southeastern part of the Baltic Sea for 2010–2019. The algorithm was verified by using the data of observations on the offshore ice-resistant stationary platform D-6, ship data obtained in the 127th cruise of the research vessel “Professor Shtokman”, and the results of upwelling detection based on the sea surface temperature derived from measurements of the MODIS Terra/Aqua spectroradiometer. It is shown that the lowest frequency of upwellings is observed in August-September (5–6 days per year), the highest — in May — June and October (11–15 days per year). In the period 2010–2013 in the study area, on average, up to 10 % of negative thermal anomalies were observed during the warm period of the year. Since 2014 (with the exception of 2017), an increase in the frequency of upwellings has been noted — on average, about 20 % of days were days with upwelling. It is shown that the winter East Atlantic/ West Russia and East Atlantic indices and the spring Scandinavia pattern index can be used to assess the characteristics of the future summer upwelling.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>прибрежный апвеллинг</kwd><kwd>температура поверхности моря</kwd><kwd>юго-восточная часть Балтийского моря</kwd></kwd-group><kwd-group xml:lang="en"><kwd>coastal upwelling</kwd><kwd>sea surface temperature</kwd><kwd>southeastern Baltic Sea</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках госзадания ИО РАН (тема № 0128–2021–0012).</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">Стонт Ж.И., Гущин О.А. Мониторинг ветровых условий в Юго-Восточной Балтике // Проблемы изучения и охраны природного и культурного наследия национального парка «Куршская коса». 2017. 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