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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/S2658697525060023</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-3043</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>СОВРЕМЕННАЯ КОЛИЧЕСТВЕННАЯ И ПРОЦЕССНАЯ ГЕОМОРФОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>MODERN QUANTITATIVE AND PROCESS GEOMORPHOLOGY</subject></subj-group></article-categories><title-group><article-title>Геоморфометрия перигляциальных территорий Антарктики</article-title><trans-title-group xml:lang="en"><trans-title>Geomorphometry of Antarctic Periglacial Territories</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>Флоринский</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Florinsky</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Пущино, Московская область</p></bio><bio xml:lang="en"><p>Pushchino, Moscow oblast</p></bio><email xlink:type="simple">iflor@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт математических проблем биологии РАН — филиал ФИЦ “Институт прикладной математики им. М.В. Келдыша РАН”</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Mathematical Problems of Biology, Keldysh Institute of Applied Mathematics, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>22</day><month>02</month><year>2026</year></pub-date><volume>89</volume><issue>6</issue><issue-title>Географические закономерности, природные и антропогенные факторы и параметры развития рельефа Северной Евразии в позднем</issue-title><fpage>884</fpage><lpage>898</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Флоринский И.В., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Флоринский И.В.</copyright-holder><copyright-holder xml:lang="en">Florinsky I.V.</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/3043">https://izvestia.igras.ru/jour/article/view/3043</self-uri><abstract><p>В современной науке строгость и воспроизводимость исследований рельефа обеспечивает геоморфометрия — дисциплина, сформировавшаяся на стыке фотограмметрии, геоинформатики и вычислительной математики, обладающая развитой физико-математической теорией и мощным вычислительным аппаратом. Методы геоморфометрии применяются для решения широкого круга разномасштабных задач наук о Земле. Геоморфометрическое моделирование перигляциальных территорий Антарктики — оазисов, свободных от оледенения островов, горных массивов и нунатаков — актуально для получения новых знаний о количественных характеристиках рельефа этих уникальных объектов и дальнейшего использования морфометрической информации. В статье рассмотрены три типичные перигляциальные антарктические территории: оазис мыса Бёркс (Земля Мэри Бэрд), остров Хасуэлл (Земля Королевы Мэри) и нунатак Ленинградский (Земля Оутса). Впервые проведено геоморфометрическое моделирование и картографирование этих территорий. В качестве исходных данных нами использованы три фрагмента цифровой модели рельефа (ЦМР) Reference Elevation Model of Antarctica (REMA) с шагом сетки 2 и 8 м. По трем ЦМР нами рассчитаны цифровые модели и представлены серии карт десяти наиболее значимых в фундаментальном и прикладном отношении морфометрических величин. К ним относятся: крутизна склона, экспозиция склона, горизонтальная кривизна, вертикальная кривизна, минимальная кривизна, максимальная кривизна, индекс ветрового воздействия, водосборная площадь, топографический индекс влажности и индекс мощности потоков. Даны интерпретации полученных карт, обсуждается их возможное использование. Работа проведена в рамках проекта по созданию физико-географического тематического научно-справочного геоморфометрического атласа свободных от оледенения территорий Антарктики.</p></abstract><trans-abstract xml:lang="en"><p>Currently, the rigor and reproducibility of topographic studies is ensured by geomorphometry. This discipline emerged at the intersection of photogrammetry, geoinformatics, and computational mathematics. It has a well-developed physical and mathematical theory, as well as a powerful computational apparatus. Geomorphometric methods are used to solve a wide range of multiscale problems within the field of geoscience. Geomorphometric modeling of Antarctic periglacial territories, such as oases, ice-free islands and mountains, is necessary to obtain new knowledge about quantitative characteristics of the topography of these unique territories as well as further use of morphometric information. This article considers three typical Antarctic periglacial territories: the Cape Burks Oasis (Marie Byrd Land), Haswell Island (Queen Mary Land), and Leningradsky Nunatak (Oates Land). Geomorphometric modelling and mapping of these territories were carried out for the first time. We used three fragments of the Reference Elevation Model of Antarctica (REMA) as input data, with grid spacings of 2 and 8 metres. We calculated digital models using three DEMs and presented a series of maps of the ten most important morphometric variables in fundamental and applied terms. The list of variables includes slope gradient, slope aspect, horizontal curvature, vertical curvature, minimal curvature, maximal curvature, wind exposition index, catchment area, topographic wetness index, and stream power index. Interpretations of the obtained maps are given and their possible use is described. The study was carried out within the framework of a project to create a physical-geographical thematic scientific reference geomorphometric atlas of ice-free territories of the Antarctic.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>рельеф</kwd><kwd>цифровое моделирование рельефа</kwd><kwd>геоморфометрическое картографирование</kwd><kwd>Антарктика</kwd><kwd>антарктический оазис</kwd><kwd>нунатак</kwd></kwd-group><kwd-group xml:lang="en"><kwd>topography</kwd><kwd>digital terrain modeling</kwd><kwd>geomorphometry</kwd><kwd>Antarctica</kwd><kwd>Antarctic oasis</kwd><kwd>nunatak</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">Абакумов Е.В., Помелов В.Н., Крыленков В.А., Власов Д.Ю. Морфологическая организация почв Западной Антарктики // Вестн. СПб. ун-та. Серия 3: Биология. 2008. Вып. 3. 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