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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">10.24057/2071-9388-2021-039</article-id><article-id custom-type="elpub" pub-id-type="custom">gesj-1891</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>Special Issue "Permafrost regions in transition"</subject></subj-group></article-categories><title-group><article-title>Landscape Indication Of Permafrost Conditions For Geoecological Assessment &amp; Mapping At Various Scales</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>Zotova</surname><given-names>Larisa I.</given-names></name></name-alternatives><bio xml:lang="en"><p>Faculty of Geography </p><p>Moscow 119991</p></bio><email xlink:type="simple">zotlar@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>15</day><month>07</month><year>2021</year></pub-date><volume>14</volume><issue>4</issue><fpage>33</fpage><lpage>40</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Zotova L.I., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Zotova L.I.</copyright-holder><copyright-holder xml:lang="en">Zotova L.I.</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/1891">https://ges.rgo.ru/jour/article/view/1891</self-uri><abstract><p>In this paper, the features of landscape indication of permafrost characteristics required for assessing the environmental state at various research scales are discussed. A number of permafrost characteristics affect the geoecological state and stability of natural landscapes, especially in the context of climate warming and technogenic surface disturbances. These include the distribution, temperature regime, thickness and cryogenic structure of permafrost, seasonal freezing and thawing, as well as the development of cryogenic processes. Their determination through the landscape view, however, is ambiguous. The choice of certain permafrost characteristics for geoecological assessment is based on many years of experience in creating cryo-ecological maps on a landscape basis by the school of Faculty of Geography, Moscow State University. The recent studies on the identification of regional cryoindicators are analyzed, including the issues of cryogenic landscapes classification and clarification of the boundaries of geocryological zones using the landscape structural method. The content of the two maps, «Permafrost Landscape Differentiation Map of the Russia Cryolithozone» at a scale of 1: 15,000,000 and «Permafrost Landscape Map of the Republic of Sakha (Yakutia)» at a scale of 1: 1,500,000, is presented, as well as their use as a basis for environmental planning and geoecological assessment.</p></abstract><kwd-group xml:lang="en"><kwd>permafrost</kwd><kwd>cryolithozone</kwd><kwd>landscape indication</kwd><kwd>cryogenic processes</kwd><kwd>geoecological mapping</kwd></kwd-group><funding-group><funding-statement xml:lang="en">This study was supported by State Assignment «The cryosphere evolution under climate change and anthropogenic impact» No. 121051100164-0 and Russian Foundation for Basic Research No. 18-05-60080. The author expresses deep gratitude to Nelly Tumel for ideas, guidance and many years of collaboration. 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