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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">dan</journal-id><journal-title-group><journal-title xml:lang="ru">Доклады Национальной академии наук Беларуси</journal-title><trans-title-group xml:lang="en"><trans-title>Doklady of the National Academy of Sciences of Belarus</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1561-8323</issn><issn pub-type="epub">2524-2431</issn><publisher><publisher-name>The Republican Unitary Enterprise Publishing House "Belaruskaya Navuka"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.29235/1561-8323-2021-65-5-618-627</article-id><article-id custom-type="elpub" pub-id-type="custom">dan-1013</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>НАУКИ О ЗЕМЛЕ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>EARTH SCIENCES</subject></subj-group></article-categories><title-group><article-title>Пространственно-временные изменения начальной фазы современного потепления климата</article-title><trans-title-group xml:lang="en"><trans-title>Space-time changes in the initial phase of modern climate warming</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>Лысенко</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Lysenko</surname><given-names>S. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Лысенко Сергей Александрович – д-р физ.-мат. наук, профессор, директор</p><p>ул. Ф. Скорины, 10, 220114, Минск</p></bio><bio xml:lang="en"><p>Lysenko Sergey A. – D. Sc. (Physics and Mathematics), Professor, Director</p><p>10, F. Skorina Str., 220114, Minsk</p></bio><email xlink:type="simple">lysenkorfe@gmail.com</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>Логинов</surname><given-names>В. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Loginov</surname><given-names>V. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Логинов Владимир Федорович – академик, д-р географ. наук, профессор, гл. науч. сотрудник</p><p>ул. Ф. Скорины, 10, 220114, Минск</p></bio><bio xml:lang="en"><p>Loginov Vladimir F. – Academician, D. Sc. (Geography), Professor, Chief researcher</p><p>10, F. Skorina Str., 220114, Minsk</p></bio><email xlink:type="simple">nature@ecology.basnet.by</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт природопользования Национальной академии наук Беларуси</institution></aff><aff xml:lang="en"><institution>Institute for Nature Management of the National Academy of Sciences of Belarus</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>08</day><month>11</month><year>2021</year></pub-date><volume>65</volume><issue>5</issue><fpage>618</fpage><lpage>627</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лысенко С.А., Логинов В.Ф., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Лысенко С.А., Логинов В.Ф.</copyright-holder><copyright-holder xml:lang="en">Lysenko S.A., Loginov V.F.</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://doklady.belnauka.by/jour/article/view/1013">https://doklady.belnauka.by/jour/article/view/1013</self-uri><abstract><p>Исследована начальная фаза современного потепления в разных районах Земного шара. Установлено, что в материковых районах потепление началось на 6–8 лет раньше, чем в океанических. В области субполярного циклонического круговорота в Северной Атлантике потепление началось лишь с наступлением положительной квази-30-летней фазы Атлантической мультидекадной осцилляции (АМО) – с 2000-х годов. На основе спектрального сингулярного анализа временного ряда температуры воздуха выделены материковые регионы, в которых летняя температура воздуха в масштабах десятилетий изменяется синхронно с АМО. В этих районах потепление также началось с запаздыванием на 10–15 лет от остальных материковых районов. Наиболее высокий уровень статистической значимости корреляции между квази-60-летними компонентами АМО и летней температуры воздуха отмечается для центральной и восточной Европы (35–60° с. ш., 10–45° в. д.). В Беларуси этим колебанием объясняется междесятилетняя изменчивость летней температуры в пределах ±(0,5–0,6) °С. На восходящей ветви АМО происходит усиление интенсивности потепления климата в летнее время года, а на нисходящей, наступившей примерно с 2010 г., – следует ожидать снижение скорости роста летних температур.</p></abstract><trans-abstract xml:lang="en"><p>The initial phase of a temperature growth in different parts of the Earth has been examined. It is found that climate warming in the continental areas began 6–8 years earlier than in the oceanic areas. Climate warming in the sub-polar cyclonic circulation area in the North Atlantic has been started only after the beginning of the positive quasi-30-year phase of the Atlantic Multidecadal Oscillation (AMO), i. e. since 2000s. On the basis of the Singular Spectrum Analysis of the air temperature time series the continental areas are found, in which summer air temperature changes are synchronous with AMO on a decadal scale. In those regions, climate warming began with a 10–15 year lag in comparison to other continental areas. The highest level of statistical significance of the correlation between quasi-60-year AMO components and summer air temperatures is observed in Central and Eastern Europe (35–60° N, 10–45° E). This oscillation explains the decadal summer temperature changes within the range of ±(0.5–0.6) °C in Belarus. Climate warming intensifies in summer during the ascending AMO segment, while during the descending segment, which has started since around 2010, the decrease in the rate of growth of summer temperatures should be expected.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>современное потепление</kwd><kwd>Атлантическая мультидекадная осцилляция</kwd><kwd>океан</kwd><kwd>квазишестидесятилетний цикл</kwd></kwd-group><kwd-group xml:lang="en"><kwd>modern warming</kwd><kwd>Atlantic Multidecadal Oscillation</kwd><kwd>ocean</kwd><kwd>quasi-60-year cycle</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Груза, Г. В. Наблюдаемые и ожидаемые изменения климата России: температура воздуха / Г. В. Груза, Э. Я. Ранькова. – М., 2012. – 194 с.</mixed-citation><mixed-citation xml:lang="en">Gruza G. V., Ran’kova E. Ya. Observed and expected climate changes in Russia: air temperature. 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