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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">10.1134/S2587556618050060</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-767</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>Природопользование и геоэкология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Natural Recourse Use and Geoecology</subject></subj-group></article-categories><title-group><article-title>ГИДРОЛОГИЧЕСКИЕ ИЗМЕНЕНИЯ В РЕГИОНАХ РУССКОЙ РАВНИНЫ В ТЕПЛЫЕ ЭПОХИ ГЕОЛОГИЧЕСКОГО ПРОШЛОГО И СЦЕНАРНОГО БУДУЩЕГО</article-title><trans-title-group xml:lang="en"><trans-title>Hydrological changes in regions of the Russian Plain in warm epochs of the geological past and the scenario future</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>Георгиади</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Georgiadi</surname><given-names>A. G.</given-names></name></name-alternatives><email xlink:type="simple">galex50@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>Милюкова</surname><given-names>И. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Milyukova</surname><given-names>I. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кашутина</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kashutina</surname><given-names>E. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии РАН, Москва</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Geography, Russian Academy of Sciences, Moscow</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>22</day><month>11</month><year>2018</year></pub-date><volume>0</volume><issue>5</issue><fpage>70</fpage><lpage>80</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Георгиади А.Г., Милюкова И.П., Кашутина Е.А., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Георгиади А.Г., Милюкова И.П., Кашутина Е.А.</copyright-holder><copyright-holder xml:lang="en">Georgiadi A.G., Milyukova I.P., Kashutina 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/767">https://izvestia.igras.ru/jour/article/view/767</self-uri><abstract><p>Выявлены особенности изменений речного стока Волги и Дона и водного баланса естественных ландшафтов Центральной лесостепи Русской равнины в позднеатлантический оптимум и в сценарных условиях потепления климата текущего столетия. Были использованы палеоклиматические реконструкции, основанные на данных спорово-пыльцевого анализа ископаемых растений и на расчетах, проведенных на ансамбле глобальных климатических моделей программы PMIP-II; а также сценарии потепления климата, выполненные на ансамбле глобальных климатических моделей программ CMIP3 и CMIP5. Гидрологические изменения оценивались на основе модели месячного водного баланса и модели влагопереноса в системе “почва–растительность–приземный слой атмосферы”. Показано, что наиболее заметные изменения речного стока Волги и Дона проявляются в трансформации характера его внутригодового распределения. Ощутимый рост температуры воздуха на фоне малозаметного изменения атмосферных осадков в рассматриваемые периоды в условиях Центральной лесостепи Русской равнины не приводит к сколько-нибудь значимым изменениям составляющих водного баланса лесных и степных ландшафтов в период вегетации.</p></abstract><trans-abstract xml:lang="en"><p>The features of the Volga and the Don river runoff changes and the water balance of the natural landscapes of the Central forest steppe of the Russian Plain during the Late Holocene Optimum and scenario conditions of global climate warming in the current century were revealed. Paleoclimatic reconstructions based on data of spore and pollen analysis of fossil plants and on calculations carried out on the ensemble of global climate models of PMIP-II program, as well as scenarios of climate warming, performed on an ensemble of global climate models of CMIP3 and CMIP5 programs, were used. Hydrological changes were evaluated on the basis of the monthly water balance and SVAT models. It is shown that the most significant changes of the Volga and Don river runoff are detected in changing the nature of its intra-annual distribution. In studied periods, the notable increase in air temperature against a backdrop of insignificant changes of atmospheric precipitation in Central forest steppe conditions of the Russian Plain does not lead to any significant changes in the water balance components of forest and steppe landscapes in growth season.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Волга</kwd><kwd>Дон</kwd><kwd>Центральная лесостепь</kwd><kwd>позднеатлантический оптимум голоцена</kwd><kwd>глобальное потепление климата</kwd><kwd>гидрологические изменения</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Volga River</kwd><kwd>Don River</kwd><kwd>Central forest steppe</kwd><kwd>Late Holocene Optimum</kwd><kwd>global climate warming</kwd><kwd>hydrological changes</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">Будаговский А.И. Уточнение моделей испарения почвенных вод // Водные ресурсы. 1986. № 5. 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