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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Bulletin of the RAS. Geography</journal-id><journal-title-group><journal-title xml:lang="en">Bulletin of the RAS. Geography</journal-title><trans-title-group xml:lang="ru"><trans-title>Известия РАН. Серия географическая</trans-title></trans-title-group></journal-title-group><issn publication-format="print">2587-5566</issn><issn publication-format="electronic">2658-6975</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">660854</article-id><article-id pub-id-type="doi">10.31857/S2587556624030052</article-id><article-id pub-id-type="edn">SOKVII</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Landscapes and Ecosystems under Climate Change</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>ЛАНДШАФТЫ И ЭКОСИСТЕМЫ В УСЛОВИЯХ МЕНЯЮЩЕГОСЯ КЛИМАТА</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Structure and Dynamics of <italic>Pinus sibirica</italic> Du Tour Forest Stands at the Upper Limit of Their Growth in the Western Part of the Katunsky Range (Altai) under Climate Change</article-title><trans-title-group xml:lang="ru"><trans-title>Структура и динамика древостоев <italic>Pinus sibirica</italic> Du Tour на верхнем пределе их произрастания в западной части Катунского хребта (Алтай) в условиях климатических изменений</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Grigoriev</surname><given-names>A. A.</given-names></name><name xml:lang="ru"><surname>Григорьев</surname><given-names>А. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Vyukhin</surname><given-names>S. O.</given-names></name><name xml:lang="ru"><surname>Вьюхин</surname><given-names>С. О.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Shalaumova</surname><given-names>Yu. V.</given-names></name><name xml:lang="ru"><surname>Шалаумова</surname><given-names>Ю. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Balakin</surname><given-names>D. S.</given-names></name><name xml:lang="ru"><surname>Балакин</surname><given-names>Д. С.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Timofeev</surname><given-names>A. S.</given-names></name><name xml:lang="ru"><surname>Тимофеев</surname><given-names>А. С.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Gromov</surname><given-names>A. M.</given-names></name><name xml:lang="ru"><surname>Громов</surname><given-names>А. М.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Golikov</surname><given-names>D. Yu.</given-names></name><name xml:lang="ru"><surname>Голиков</surname><given-names>Д. Ю.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Nizametdinov</surname><given-names>N. F.</given-names></name><name xml:lang="ru"><surname>Низаметдинов</surname><given-names>Н. Ф.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Moiseev</surname><given-names>P. A.</given-names></name><name xml:lang="ru"><surname>Моисеев</surname><given-names>П. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>grigoriev.a.a@ipae.uran.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Institute of Plant and Animal Ecology of the Ural Branch of the Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Институт экологии растений и животных Уральского отделения Российской академии наук</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Botanical Garden of the Ural Branch of the Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Ботанический сад Уральского отделения Российской академии наук</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2024-04-15" publication-format="electronic"><day>15</day><month>04</month><year>2024</year></pub-date><volume>88</volume><issue>3</issue><fpage>321</fpage><lpage>336</lpage><history><date date-type="received" iso-8601-date="2025-02-22"><day>22</day><month>02</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2024, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2024, Российская академия наук</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/2587-5566/article/view/660854">https://journals.eco-vector.com/2587-5566/article/view/660854</self-uri><abstract xml:lang="en"><p>The forest boundary is characterized by being highly sensitive to climate change. In this regard, monitoring the distribution of forested areas on the southern and northern boundaries of the forest in lowland conditions, as well as the upper and lower boundaries of the forest in mountainous regions, is one of the simplest and most effective methods for studying the response of vegetation to climate change. In the western part of the Katun Range (Central Altai), based on the use of classical dendrochronological methods, the age of 891 <italic>Pinus sibirica </italic>Du Tour trees growing at different altitudes above sea level was established. Comparison of the altitudinal position of the upper limit of tree vegetation according to topographic maps of 1956 and modern satellite images made it possible to establish the rate of change in forested areas depending on the presence or absence of edaphic restrictions for the successful regeneration of tree species. It is shown that, starting from the second half of the 20th century. There is an intensive expansion of <italic>Pinus sibirica</italic>, the most common tree species in the study area, into the belt of mountain meadows and tundras. The nature and rate of colonization by woody vegetation vary significantly depending on the exposure of the slope and its hypsometric characteristics. The closest connections were found between the appearance of cedar and climatic indicators of the cold period (temperature and precipitation), this is especially typical for slopes with northern and eastern exposures. It was shown that the expansion of the forest was favored by a general change in climatic conditions in the study area.</p></abstract><trans-abstract xml:lang="ru"><p>Граница леса характеризуется высокой чувствительную к изменениям климата. В этой связи мониторинг распределения лесопокрытых площадей на южной и северной границах леса в равнинных условиях, а также верхней и нижней границах леса в горных регионах является одним из наиболее простых и эффективных методов изучения реакции растительности на климатические изменения. В западной части Катунского хребта (Центральный Алтай) на основе использования классических методов дендрохронологии был установлен возраст 891 дерева <italic>Pinus sibirica</italic> Du Tour, произрастающих на разной высоте над уровнем моря. Сравнение высотного положения верхней границы древесной растительности по данным топографических карт 1956 г. и современных спутниковых снимков позволило установить скорость изменения лесопокрытых площадей в зависимости от наличия или отсутствия эдафических ограничений для успешного возобновления древесных видов. Показано, что, начиная со второй половины ХХ в., происходит интенсивная экспансия <italic>Pinus sibirica</italic> – наиболее распространенного в районе исследования древесного вида, в пояс горных лугов и тундр. Характер и темпы заселения древесной растительностью имеют значительные различия в зависимости от экспозиции склона и его гипсометрических характеристик. Наиболее тесные связи обнаружены между появлением кедра и климатическими показателями холодного периода (температурой и осадками), особенно это характерно для склонов северной и восточной экспозиций. Показано, что экспансии леса благоприятствовало общее изменение климатических условий в районе исследований.</p></trans-abstract><kwd-group xml:lang="en"><kwd>upper treeline</kwd><kwd>age structure of forests</kwd><kwd>topographic maps</kwd><kwd>satellite images</kwd><kwd>mountains of Southern Siberia</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>верхняя граница древесной растительности</kwd><kwd>возрастная структура древостоев</kwd><kwd>топографические карты и спутниковые изображения</kwd><kwd>горы Южной Сибири</kwd></kwd-group><funding-group><award-group><funding-source><institution-wrap><institution xml:lang="ru">Российский научный фонд</institution></institution-wrap><institution-wrap><institution xml:lang="en">Russian Science Foundation</institution></institution-wrap></funding-source><award-id>21-14-00137</award-id></award-group></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><citation-alternatives><mixed-citation xml:lang="en">Büntgen U., Hellmann L., Tegel W., Normand S., Myers-Smith I., Kirdyanov A.V., Nievergelt D., Schweingruber F.H. 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