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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="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gesj</journal-id><journal-title-group><journal-title xml:lang="en">GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</journal-title><trans-title-group xml:lang="ru"><trans-title>GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2071-9388</issn><issn pub-type="epub">2542-1565</issn><publisher><publisher-name>Russian Geographical Society</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24057/2071-9388-2018-42</article-id><article-id custom-type="elpub" pub-id-type="custom">gesj-659</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="en"><subject>RESEARCH PAPER</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Статьи</subject></subj-group></article-categories><title-group><article-title>Estimation of Dispersed Glaciation Shrinkage Under Climate Change</article-title><trans-title-group xml:lang="ru"><trans-title></trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Glazirin</surname><given-names>Gleb E.</given-names></name></name-alternatives><bio xml:lang="en"><p>Gleb E. Glazirin - Faculty of Geography.</p><p>Tashkent</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Semakova</surname><given-names>Eleonora R.</given-names></name></name-alternatives><bio xml:lang="en"><p>Eleonora R. Semakova - Faculty of Geography.</p><p>Tashkent</p></bio><email xlink:type="simple">ella9sem@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>National University of Uzbekistan</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>28</day><month>03</month><year>2019</year></pub-date><volume>12</volume><issue>1</issue><fpage>5</fpage><lpage>12</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Glazirin G.E., Semakova E.R., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Glazirin G.E., Semakova E.R.</copyright-holder><copyright-holder xml:lang="en">Glazirin G.E., Semakova E.R.</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://ges.rgo.ru/jour/article/view/659">https://ges.rgo.ru/jour/article/view/659</self-uri><abstract><p>We propose a new method of estimating the shrinkage of glaciers over a wide area under conditions of changed climate. The method can be also used to quantitatively estimate the presence of glaciers under past climatic conditions, in mountainous areas where they are currently absent. The method is based on the use of statistical parameters of the distribution of glaciers by altitude zones, according to vertical distance from the climatic equilibrium line altitude (CELA). The method was used for the Pskem River basin (tributary of the Chirchik River, Western Tien-Shan) where glaciation has been extensively studied. Data are available for several glacier inventories for the basin for different time periods from 1957 to 2010. The number of glaciers for the part of the basin considered in the studies decreased by 16 percent during that period. Mean summer air temperature and annual precipitation were used as climate indicators characterizing ablation and accumulation on glaciers. Data of several meteorological stations located in the Pskem River basin were used to document these climatic characteristics. We estimated shrinkage of glaciers over the area for increases of summer air temperature of 0.5 - 2°C.</p></abstract><kwd-group xml:lang="en"><kwd>glaciers distribution</kwd><kwd>glaciation shrinkage</kwd><kwd>climate change</kwd></kwd-group><funding-group><funding-statement xml:lang="en">L.N. Borovikova, Dr.; Todd K.,Dr.</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">Borovikova L., Denisov Yu., Trofimova E. and Shentsis I. (1972). Mathematical modeling of the flow process of mountain rivers. Leningrad: Gidrometeoizdat. (In Russian).</mixed-citation><mixed-citation xml:lang="en">Borovikova L., Denisov Yu., Trofimova E. and Shentsis I. (1972). Mathematical modeling of the flow process of mountain rivers. Leningrad: Gidrometeoizdat. 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