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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/S2587556621010131</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-1288</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>Эволюция природных систем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Evolution of Natural System</subject></subj-group></article-categories><title-group><article-title>Пространственно-временной анализ формирования узких годичных колец сосны ленточных боров степной зоны Западной Сибири</article-title><trans-title-group xml:lang="en"><trans-title>Spatiotemporal Analysis of the Formation of Narrow Tree-Rings of Pine Belt Forests in the Steppe Zone of Western Siberia</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>Рыгалова</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Rygalova</surname><given-names>N. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Барнаул</p></bio><bio xml:lang="en"><p>Barnaul</p></bio><email xlink:type="simple">natalia.ml@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Харламова</surname><given-names>Н. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Kharlamova</surname><given-names>N. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Барнаул</p></bio><bio xml:lang="en"><p>Barnaul</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Алтайский государственный университет<country>Россия</country></aff><aff xml:lang="en">Altai State University<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>09</day><month>06</month><year>2021</year></pub-date><volume>85</volume><issue>1</issue><fpage>109</fpage><lpage>119</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Рыгалова Н.В., Харламова Н.Ф., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Рыгалова Н.В., Харламова Н.Ф.</copyright-holder><copyright-holder xml:lang="en">Rygalova N.V., Kharlamova N.F.</copyright-holder><license 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/1288">https://izvestia.igras.ru/jour/article/view/1288</self-uri><abstract><p>В данной статье изложены результаты исследования узких годичных колец сосны обыкновенной (Pinus sylvestris L.) ленточных боров (юг Западной Сибири) в степной зоне за период с 1661 по 2019 г. В анализе использованы 19 древесно-кольцевых хронологий, полученных по кернам живых деревьeв и исторической древесины старых сельских домов. Узкие кольца у 75% всех хронологий были отмечены в 2012, 2003, 1996, 1991, 1980, 1974, 1963, 1910, 1896, 1888, 1812, 1795, 1786, 1752, 1748, 1695, 1690 и 1688 гг., которые могут быть определены как региональные реперные годы. Отмечается увеличение частоты формирования минимумов радиального прироста во второй половине ХХ в., а также во второй половине XVIII — начале XIX в., а снижение частоты — в конце XVII — начале XVIII в. В годы формирования узких колец почти в 100% случаев отмечается засуха в весенне-летний период (особенно в мае), также значим дефицит осадков в предшествующий осенне-зимний сезон. Установлено, что максимальная концентрация минимумов прироста сосны приходится на периоды преобладания южных меридиональных циркуляционных эпох.</p></abstract><trans-abstract xml:lang="en"><p>This article presents the results of the study of narrow pine tree-rings (Pinus sylvestris L.) of the belt forests (south of Western Siberia) in the steppe zone for the period from 1661 to 2019. In the analysis 19 tree-ring chronologies obtained from living trees and historical wood of old rural houses have been used. Narrow tree-rings in 75% of all chronologies have been noted for 2012, 2003, 1996, 1991, 1980, 1974, 1963, 1910, 1896, 1888, 1812, 1795, 1786, 1752, 1748, 1695, 1690 and 1688, which can be defined as regional pointer years. The increase in the frequency of formation of minimum radial growth in the second half of the 20th century, as well as in the second half of the 18th-early 19th centuries has been distinguished. The minimum number of narrow rings falls on the end of the 17th century-the beginning of the 18th century. Drought in the spring and summer period (especially in May) has been observed in the years of narrow rings formation in almost 100% of cases. Also significant is the deficit of precipitation in the preceding autumn-winter season. It has been established that the maximum concentration of pine growth minima falls on the periods of dominance of southern meridional circulation epochs.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>узкие годичные кольца</kwd><kwd>сосна обыкновенная</kwd><kwd>древесно-кольцевая хронология</kwd><kwd>ленточные боры</kwd><kwd>историческая древесина</kwd><kwd>засухи</kwd><kwd>засушливые территории</kwd><kwd>циркуляционные эпохи</kwd><kwd>реперный год</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Narrow tree-rings</kwd><kwd>Scots pine</kwd><kwd>tree-ring chronology</kwd><kwd>pine belt forests</kwd><kwd>historical wood</kwd><kwd>drought</kwd><kwd>semi-arid territory</kwd><kwd>circulation epochs</kwd><kwd>pointer year</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Публикация подготовлена при финансовой поддержке РФФИ в рамках реализации проекта № 18-05-00694_а</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>The study was financially supported by the Russian Foundation for Basic Research (project no. 18-05-00694_а)</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">Алтайский край. 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