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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">10.31857/S2587556620030115</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-1091</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>Тепловое воздействие на территории России в середине XXI века по модельным данным</article-title><trans-title-group xml:lang="en"><trans-title>Thermal Impact in the Territory of Russia in the Middle of the 21st Century by Model Data</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>Виноградова</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Vinogradova</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"><p>Moscow</p></bio><email xlink:type="simple">vvvinog@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт географии, РАН<country>Россия</country></aff><aff xml:lang="en">Institute of Geography, Russian Academy of Sciences<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>29</day><month>06</month><year>2020</year></pub-date><volume>84</volume><issue>3</issue><fpage>404</fpage><lpage>413</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Виноградова В.В., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Виноградова В.В.</copyright-holder><copyright-holder xml:lang="en">Vinogradova V.V.</copyright-holder><license 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/1091">https://izvestia.igras.ru/jour/article/view/1091</self-uri><abstract><p>Оценка изменения частоты, интенсивности и продолжительности волн тепла в летний период (июнь-август) на территории России для “исторического периода” (1980—1999 гг.) и прогноза на середину XXI в. (2046—2055 гг.) проводилась по данным, полученным на глобальной климатической модели (INMCM4) Института вычислительной математики РАН. Определение критериев экстремальных явлений зависит от выбора пороговых значений. В настоящей работе рассматриваются пороговые значения для определения волн тепла как значения 95-й процентили распределения максимальной суточной температуры. Анализ полученных результатов показывает, что при “мягком” сценарии RCP4.5 в середине XXI в. ожидается увеличение числа дней с максимальными температурами, превышающими пороговые значения на юге Европейской территории России и Западной Сибири, в Якутии, на севере Чукотки и в Приморском крае. Максимальные изменения ожидаются на Таймыре и Ямале. На остальной территории число таких дней может сократиться. Для “жесткого” сценария RCP8.5 ожидаются более контрастные изменения при сохранении основных особенностей их локализации. При этом сценарии в середине XXI в. на юге страны средняя максимальная температура в волне тепла может превысить 40 °С.</p></abstract><trans-abstract xml:lang="en"><p>The assessment of heat waves’ number, intensity and duration change during summer (June-August) in the Russia territory for the “historical period” (1980-1999) and for the middle of the 21st century (2046-2055) was made according to the data of the global climate model (INMCM4) of the Institute of Numerical Mathematics, Russian Academy of Sciences. The definition of the extreme events’ criteria depends on the thresholds’ choice. In this paper, heat waves’ thresholds are considered as the values of the 95th percentile of maximum daily temperature distribution. An increase in the number of days with maximum temperatures exceeding the threshold values for the south of the European Russia and Western Siberia, Yakutia, the north of Chukotka, and Primorsky krai in the middle of the 21st century according to the “soft” scenario of RCP4.5 was revealed. Maximum changes are expected in Taimyr and Yamal. In the rest of the territory, the number of such days will be reduced. For the “hard” scenario of RCP8.5, more contrast changes in the similar locations are expected. Under the “hard” scenario, by the middle of the 21st century the maximum temperature in the heat wave will exceed 40°C in the south of the country.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>волны тепла</kwd><kwd>максимальная суточная температура</kwd><kwd>дискомфорт</kwd><kwd>пороговые значения</kwd><kwd>потепление климата</kwd><kwd>модельные прогнозы</kwd></kwd-group><kwd-group xml:lang="en"><kwd>heat waves</kwd><kwd>maximum daily temperature</kwd><kwd>discomfort</kwd><kwd>thresholds</kwd><kwd>climate warming</kwd><kwd>model forecasts</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Исследование выполнено за счет гранта Российского научного фонда (проект № 16-17-10236)</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>The study was financially supported by the Russian Science Foundation, project no. 16-17-10236</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">Виноградова В.В. 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