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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">nature</journal-id><journal-title-group><journal-title xml:lang="ru">Природопользование</journal-title><trans-title-group xml:lang="en"><trans-title>Nature Management</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2079-3928</issn><publisher><publisher-name>Институт природопользования НАН Беларуси</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">nature-80</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>ГЕОГРАФИЯ. ГЕОЭКОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOGRAPHY. GEOECOLOGY</subject></subj-group></article-categories><title-group><article-title>Оценка влияния растительного покрова  на температуру подстилающей поверхности в различных геотехнических системах г. Могилёва</article-title><trans-title-group xml:lang="en"><trans-title>Assessment of the influence of vegetation cover on  the land surface temperature for different geotechnical systems of Mogilev city</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>Кравчук</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kravchuk</surname><given-names>L. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кравчук Людмила Александровна – кандидат географических наук, доцент, ведущий научный сотрудник</p><p>ул. Ф. Скорины, 10, 220076, г. Минск</p></bio><bio xml:lang="en"><p>Lyudmila A. Kravchuk – Ph. D. (Geography), Associate Professor, Leader Researcher</p><p>10, F. Skoriny Str., 220076, Minsk</p></bio><email xlink:type="simple">kravchu-k@yandex.by</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>Яновский</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Yanovskiy</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Яновский Александр Александрович – кандидат технических наук, доцент, старший научный сотрудник</p><p>ул. Ф. Скорины, 10, 220076, г. Минск</p></bio><bio xml:lang="en"><p>Aleksander A. Yanovskiy – Ph. D. (Technical), Associate Professor, Senior Researcher</p><p>10, F. Skoriny Str., 220076, Minsk</p></bio><email xlink:type="simple">yanouski@ya.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>Баженова</surname><given-names>Н. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Bazhenova</surname><given-names>N. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Баженова Наталья Михайловна – научный  сотрудник</p><p>ул. Ф. Скорины, 10, 220076, г. Минск</p></bio><bio xml:lang="en"><p>Natallia M. Bazhenova – Researcher</p><p>10, F. Skoriny Str., 220076, Minsk</p></bio><email xlink:type="simple">nata.bazh@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт природопользования НАН Беларуси</institution></aff><aff xml:lang="en"><institution>Institute of Nature Management of the National Academy of Sciences of Belarus</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>03</day><month>11</month><year>2025</year></pub-date><volume>0</volume><issue>2</issue><fpage>13</fpage><lpage>23</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кравчук Л.А., Яновский А.А., Баженова Н.М., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Кравчук Л.А., Яновский А.А., Баженова Н.М.</copyright-holder><copyright-holder xml:lang="en">Kravchuk L.A., Yanovskiy A.A., Bazhenova N.M.</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://www.nature-journal.by/jour/article/view/80">https://www.nature-journal.by/jour/article/view/80</self-uri><abstract><p>С использованием данных дистанционного зондирования Земли (ДЗЗ) и ГИС-проекта территории г. Могилёва исследованы особенности растительного покрова города и его влияния на температуру подстилающей поверхности (LST) в различных типах геотехнических систем (ГТС) крупного города. Наименьшие средние значения LST регистрировались в лесных экосистемах г. Могилёва. За ними следуют резервные озелененные территории, расположенные преимущественно в долинах рек, далее – парки и малые ландшафтные формы. В классе застроенных территорий наиболее высокие средние значения LST относились к производственно-коммунальным ГТС, а низкие – к жилой многоквартирной, общественной застройке и участкам незавершенного строительства. Жилая усадебная застройка характеризовалась наименьшими в данном классе средними значениями LST. Показано наличие обратной связи значений LST с различными характеристиками растительного покрова, полученными по данным ДЗЗ. Коэффициенты корреляции средних значений LST cо средними значениями нормализованного разностного индекса растительности (NDVI), индекса листовой поверхности (LAI), содержания в пологе хлорофилла (CCC) и степенью озелененности всех выделов ГТС в городе оцениваются от –0,6 до –0,7. Более сильные обратные связи отмечены для резервных озелененных территорий, представленных преимущественно древесно-кустарниковой растительностью в долинах рек (варьируют в пределах от –0,7 до –0,8). Связи ослабевают в ГТС жилой многоквартирной застройки (до –0,5 и –0,6), ГТС производственно-коммунальных территорий (от –0,4  до –0,6) и лесах (от –0,3 до –0,6).</p></abstract><trans-abstract xml:lang="en"><p>The joint analysis of Earth remote sensing data and geographic information system (GIS) project differentiated by type of geotechnical systems (GTS) for the territory of the city of Mogilev, explored the features of the influence of vegetation cover on the land surface temperature (LST) in various types of GTS of a large city. As part of landscaperecreational territories, the lowest average LST values were recorded in forest ecosystems of the city of Mogilev. They are followed by reserved green areas, located mainly in river valleys, then – parks and small landscape forms. In the class of built-up areas, the highest average LST values were related to industrial and communal structures. They were lower in residential multi-apartment, public and in areas of unfinished construction. Residential estate was characterized by the lowest average LST. It is shown a feedback between LST and various characteristics of vegetation cover obtained from remote sensing data. Correlation of average LST with average normalized difference vegetation index (NDVI), leaf area index (LAI), canopy chlorophyll content (CCC) and the degree of greening for all type system in the city are estimated from –0.6 to –0.7. Stronger feedbacks were noted for reserved green areas (mainly by trees and shrubs in river valleys) varying from –0.7 to –0.8. The connections are weakening in the GTS of residential multi-apartment buildings (up to –0.5 and 0.6), in the GTS of industrial and communal areas (from –0.4 to –0.6) and forests (from –0.3 to –0.6).</p></trans-abstract><kwd-group xml:lang="ru"><kwd>город</kwd><kwd>геотехническая система</kwd><kwd>растительный покров</kwd><kwd>дистанционное зондирование</kwd></kwd-group><kwd-group xml:lang="en"><kwd>city</kwd><kwd>geotechnical system</kwd><kwd>vegetation cover</kwd><kwd>remote sensing</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">Нацыянальны Атлас Беларусі / Камiтэт па зямельных рэсурсах, геадэзii i картаграфii пры Савеце Мiнicтраў Рэспублiкi Беларусь. – Минск, 2002. – 292 с.</mixed-citation><mixed-citation xml:lang="en">Nacyyanal'ny Atlas Belarusі [National Atlas of Belarus]. 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