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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">sergeogr</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Российской академии наук. Серия географическая</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2587-5566</issn><issn pub-type="epub">2658-6975</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.7868/S0373244417050061</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-611</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>Природные процессы и динамика геосистем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Natural Processes and Dynamics of Geosystems</subject></subj-group></article-categories><title-group><article-title>СЕЗОННЫЕ ОСАДКИ НА ТЕРРИТОРИИ ВОСТОЧНО-ЕВРОПЕЙСКОЙ РАВНИНЫ В ПЕРИОДЫ ТЕПЛЫХ И ХОЛОДНЫХ АНОМАЛИЙ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ СЕВЕРНОЙ АТЛАНТИКИ</article-title><trans-title-group xml:lang="en"><trans-title>SEASONAL PRECIPITATION IN THE EAST EUROPEAN PLAIN DURING THE PERIODS OF WARM AND COOL ANOMALIES OF THE NORTH ATLANTIC SURFACE TEMPERATURE</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>Черенкова</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Cherenkova</surname><given-names>E. A.</given-names></name></name-alternatives><email xlink:type="simple">cherenkova@igras.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Geography, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2017</year></pub-date><pub-date pub-type="epub"><day>25</day><month>10</month><year>2017</year></pub-date><volume>0</volume><issue>5</issue><fpage>72</fpage><lpage>81</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Черенкова Е.А., 2017</copyright-statement><copyright-year>2017</copyright-year><copyright-holder xml:lang="ru">Черенкова Е.А.</copyright-holder><copyright-holder xml:lang="en">Cherenkova E.A.</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://izvestia.igras.ru/jour/article/view/611">https://izvestia.igras.ru/jour/article/view/611</self-uri><abstract><p>В статье исследованы изменения сезонных осадков на территории Восточно-Европейской равнины в периоды более теплой и более холодной Северной Атлантики в XX – начале XXI в. Установлено, что различия в распределении сезонных осадков на территории Восточно-Европейской равнины между противоположными фазами Атлантической мультидекадной осцилляции были статистически значимыми. Весной фазы более теплой Северной Атлантики (периоды 1926–1962 гг. и 1995–2012 гг.) ассоциировались с бóльшим количеством осадков в целом на Восточно-Европейской равнине, чем в более холодную ее фазу (период 1963–1994 гг.). Напротив, летом в аналогичные теплые фазы на большей части Восточно-Европейской равнины наблюдались более засушливые условия. Показано, что выявленная согласованность пространственного распределения изменений сезонных осадков в теплые фазы Северной Атлантики является следствием сходства пространственной структуры полей давления на уровне моря в Атлантико-Европейском секторе в аналогичные периоды.</p></abstract><trans-abstract xml:lang="en"><p>The seasonal precipitation changes in the East European Plain in the periods of warm and cool anomalies of North Atlantic surface temperature in the 20th – beginning of the 21st century were studied in the paper. The difference between spatial distributions of seasonal precipitation in the East European Plain in the opposite phases of Atlantic Multidecadal Oscillation was found to be significant. In spring, the warm phases of the North Atlantic (1926–1962 and 1995–2012) are associated with a larger amount of precipitation in the East European Plain in general than in cool phase (1963–1994). In contrast, in summer, drier conditions were observed in the same warm phases in the most parts of the East European Plain. It was shown that the coherence of spatial patterns of seasonal precipitation changes during the warm phases of the North Atlantic caused by their response to the similarities of the sea level pressure patterns in the Atlantic-European sector in the same periods.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>сезонные осадки</kwd><kwd>температура поверхности океана</kwd><kwd>атмосферная циркуляция</kwd><kwd>аномалии</kwd><kwd>изменение климата</kwd><kwd>Восточно-Европейская равнина</kwd><kwd>Северная Атлантика</kwd></kwd-group><kwd-group xml:lang="en"><kwd>seasonal precipitation</kwd><kwd>sea surface temperature</kwd><kwd>anomalies</kwd><kwd>atmospheric circulation</kwd><kwd>climate change</kwd><kwd>East European Plain</kwd><kwd>North Atlantic Ocean</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">Золотокрылин А.Н., Черенкова Е.А. 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