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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">aari</journal-id><journal-title-group><journal-title xml:lang="ru">Проблемы Арктики и Антарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Antarctic Research</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0555-2648</issn><issn pub-type="epub">2618-6713</issn><publisher><publisher-name>Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.30758/0555-2648-2024-70-2-161-173</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-609</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>МЕТЕОРОЛОГИЯ И КЛИМАТОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>METEOROLOGY AND CLIMATOLOGY</subject></subj-group></article-categories><title-group><article-title>Некоторые механизмы формирования аномальной температуры воздуха в летние сезоны на арх. Шпицберген</article-title><trans-title-group xml:lang="en"><trans-title>Some mechanisms of abnormal surface air temperature formation in the area of the Spitsbergen archipelago in summer</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0006-9643-3063</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Ильющенкова</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ilyushchenkova</surname><given-names>I. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Irina A. Ilyushchenkova</p><p>St. Petersburg</p></bio><email xlink:type="simple">ilyushenkova@aari.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/0009-0004-2610-450X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Коржиков</surname><given-names>А. Я.</given-names></name><name name-style="western" xml:lang="en"><surname>Korzhikov</surname><given-names>A. Ya.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Alexander Ya. Korzhikov</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-6801-5458</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Иванов</surname><given-names>Б. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>B. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Boris V. Ivanov</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт; Санкт-Петербургский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute; Saint-Petersburg State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>27</day><month>06</month><year>2024</year></pub-date><volume>70</volume><issue>2</issue><fpage>161</fpage><lpage>173</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ильющенкова И.А., Коржиков А.Я., Иванов Б.В., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Ильющенкова И.А., Коржиков А.Я., Иванов Б.В.</copyright-holder><copyright-holder xml:lang="en">Ilyushchenkova I.A., Korzhikov A.Y., Ivanov B.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://www.aaresearch.science/jour/article/view/609">https://www.aaresearch.science/jour/article/view/609</self-uri><abstract><p>.</p><p>Исследованы особенности формирования летних аномальных значений приземной температуры воздуха в районе арх. Шпицберген. В работе использован временной ряд среднемесячных величин приземной температуры воздуха в п. Баренцбург с 1912 по 2023 г. Выявлены значимые различия в характере атмосферной циркуляции, соответствующей аномально теплым и холодным летним сезонам, и рассчитаны корреляционные связи с индексами атмосферной циркуляции. Наибольшая статистически значимая связь аномалий приземной температуры воздуха наблюдается с индексом Арктический диполь, теснота связи в сентябре составила –0,49. Проведен спектральный анализ временных рядов индексов атмосферной циркуляции и определены основные периоды колебаний от 2–3 лет до 25 лет.</p></abstract><trans-abstract xml:lang="en"><p>The temperature in the Arctic is increasing faster than the global average. A question that challenges scientific community is whether the intensity and frequency of dangerous meteorological phenomena in the Arctic are increasing as rapidly. The article presents the results of examining abnormal summer seasons in the area of the Spitsbergen archipelago. The study used data on surface air temperature in Barentsburg obtained from 1912 to 2023. The regional average results showed a statistically significant linear summer trend. The mean summer temperature in Barentsburg is increasing at a rate of 0.2 °C/10 years. Positive and negative extremes of seasonal mean temperature in the summer from June to September were determined as higher than or equal to 1,5 standard deviation. The atmospheric circulation at the sea level pressure and at the height of the geopotential surface of 500 hPa is analyzed, and the localization of surface temperatures anomalies for highlighted abnormal temperature in summer season events is discussed. The results of the analysis of atmospheric circulation revealed significant differences between abnormal warm and cold summer seasons. During abnormally cold summers the circumpolar vortex is located in the polar region and causes the advection of cold air masses from the north of Greenland. In the case of abnormally warm summers the cyclonic vortex is shifted to the Canadian Arctic archipelago and the Baffin Sea, while warm air masses from the Atlantic Ocean enter the area of the Spitsbergen archipelago. The assessment of the statistical significance of the correlation between the time series of surface air temperature anomalies and the atmospheric circulation indices Arctic Oscillation, Arctic dipole, Pacific North American oscillation showed significant results in September with the Arctic Oscillation index, in August and September with the Arctic dipole index, in July with the Pacific North American oscillation index. The greatest statistically significant association of surface air temperature anomalies was found with the Arctic dipole index, the closeness of the connection in September was –0.49. Spectral analysis was carried out and the main periods of atmospheric indices fluctuations from 2–3 years to 25 years were determined.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>атмосферная циркуляция</kwd><kwd>Западная Арктика</kwd><kwd>приземная температура воздуха</kwd><kwd>современное потепление</kwd><kwd>циркумполярный вихрь</kwd><kwd>Шпицберген</kwd></kwd-group><kwd-group xml:lang="en"><kwd>air temperature</kwd><kwd>atmospheric circulation</kwd><kwd>polar vortex</kwd><kwd>recent warming</kwd><kwd>Spitsbergen</kwd><kwd>Western Arctic</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при поддержке гранта РНФ № 24-27-00112 «Современные изменения арктического климата и экстремальные колебания погоды в западном секторе Северного морского пути»</funding-statement><funding-statement xml:lang="en">This study was made within the framework of Russian Science Foundation grant 24-27-00112 “Current changes in the Arctic climate and extreme weather fluctuations in the western sector of the Northern Sea Route”</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">Третий оценочный доклад об изменениях климата и их последствиях на территории Российской Федерации. 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