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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/S2587556623010089</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-1734</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>Геоинформационные системы и картографирование</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Geoinformation Systems and Mappings</subject></subj-group></article-categories><title-group><article-title>Распознавание образов в задачах картографирования рельефа суши</article-title><trans-title-group xml:lang="en"><trans-title>Pattern Recognition in the Tasks of Landform Mapping</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>Харченко</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kharchenko</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Москва</p></bio><bio xml:lang="en"><p>Moscow</p></bio><email xlink:type="simple">xar4enkkoff@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова; Институт географии РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Moscow State University; Institute of Geography, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>16</day><month>04</month><year>2023</year></pub-date><volume>87</volume><issue>1</issue><fpage>192</fpage><lpage>206</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Харченко С.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Харченко С.В.</copyright-holder><copyright-holder xml:lang="en">Kharchenko S.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/1734">https://izvestia.igras.ru/jour/article/view/1734</self-uri><abstract><p>В статье рассмотрено современное состояние методов распознавания образов для автоматического и полуавтоматического составления геоморфологических карт. В настоящее время среди специалистов в области морфометрии и математического моделирования рельефа широко распространено мнение, что экспертные знания и правила, используемые для создания таких карт, могут быть описаны количественно и представлены алгоритмически. Основные нерешенные пока удовлетворительно проблемы автоматизации картографирования рельефа: распознавание морфологически идентичных форм разного генезиса, выработка критериев перехода от морфологических к возрастным и генетическим характеристикам поверхностей, превентивный подбор оптимальной детальности данных дистанционного зондирования (не всегда наиболее детальные данные оказываются эффективнее всего в модели), выбор и обоснование весовых коэффициентов количественных переменных. Приведены примеры использования нескольких методов распознавания образов в геоморфологии вообще и геоморфологическом картографировании: обобщенных линейных моделей, классификаций деревьев решений, искусственных нейронных сетей и некоторых других методов, включая “компьютерное зрение”. Показано, что точность различных моделей в отношении распознавания форм рельефа (равно как и геологических структур) составляет порядка 50–70%, реже больше. В то же время распознавание конкретных форм, в зависимости от исходных данных и степени выраженности на них признаков данных форм рельефа, может иногда быть даже абсолютной (100%), но чаще всего точность при тестировании находится в пределах 90%.</p></abstract><trans-abstract xml:lang="en"><p>The article aims to show the modern state of pattern recognition techniques for automatic and semi-automatic geomorphological mapping. There is opinion among the geomorphometrists about the expert rules for traditional landform mapping can be quantitated. The general unsolved tasks of automatic landform mapping are: recognition of origin for morphologically similar Earth’s surface forms; criteria development for transfer from morphological to genetic and age landform’s characteristics; preventive choosing the optimal resolution of the remote sensing data; the choosing and rationale of predictor’s weights in statistical modeling procedures. Some cases of the pattern recognition techniques using in geomorphology and landform mapping are given: generalized linear models; classification trees; random forest; artificial neural networks; and computer vision methods. The overall accuracy of the different models according to planar continuous landform recognition (and recognition of lithology types too) is about 50–70% and more. At the same time, specific landform type’s (craters, volcanic cones and others) recognition can reach 90–100%.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>распознавание образов</kwd><kwd>геоморфологическое картографирование</kwd><kwd>классификация с обучением</kwd><kwd>анализ изображений</kwd></kwd-group><kwd-group xml:lang="en"><kwd>pattern recognition</kwd><kwd>geomorphological mapping</kwd><kwd>supervised classification</kwd><kwd>image analysis</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено за счет гранта Российского научного фонда (проект № 19-77-10036)</funding-statement><funding-statement xml:lang="en">The study was supported by the Russian Science Foundation (project no. 19-77-10036)</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">Гаврилов А.А. 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