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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="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gesj</journal-id><journal-title-group><journal-title xml:lang="en">GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</journal-title><trans-title-group xml:lang="ru"><trans-title>GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2071-9388</issn><issn pub-type="epub">2542-1565</issn><publisher><publisher-name>Russian Geographical Society</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24057/2071-9388-2016-9-4-17-23</article-id><article-id custom-type="elpub" pub-id-type="custom">gesj-114</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="en"><subject>ENVIRONMENT</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Окружающая среда</subject></subj-group></article-categories><title-group><article-title>WARMER URBAN CLIMATES FOR DEVELOPMENT OF GREEN SPACES IN NORTHERN SIBERIAN CITIES</article-title><trans-title-group xml:lang="ru"><trans-title></trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Esau</surname><given-names>Igor</given-names></name></name-alternatives><bio xml:lang="en"><p>Thormohlensgt. 47, 5006, Bergen</p></bio><email xlink:type="simple">igore@nersc.no</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Miles</surname><given-names>Victoria</given-names></name></name-alternatives><bio xml:lang="en"><p>Thormohlensgt. 47, 5006, Bergen</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Nansen Environmental and Remote Sensing Center/Bjerknes Centre for Climate Research</institution><country>Norway</country></aff><pub-date pub-type="collection"><year>2016</year></pub-date><pub-date pub-type="epub"><day>01</day><month>12</month><year>2016</year></pub-date><volume>9</volume><issue>4</issue><fpage>48</fpage><lpage>62</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Esau I., Miles V., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Esau I., Miles V.</copyright-holder><copyright-holder xml:lang="en">Esau I., Miles 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://ges.rgo.ru/jour/article/view/114">https://ges.rgo.ru/jour/article/view/114</self-uri><abstract><p>Modern human societies have accumulated considerable power to modify their environment and the earth’s system climate as the whole. The most significant environmental changes are found in the urbanized areas. This study considers coherent changes in vegetation productivity and land surface temperature (LST) around four northern West Siberian cities, namely, Tazovsky, Nadym, Noyabrsk and Megion. These cities are located in tundra, forest-tundra, northern taiga and middle taiga bioclimatic zones correspondingly. Our analysis of 15 years (2000–2014) Moderate Resolution Imaging Spectroradiometer (MODIS) data revealed significantly (1.3 °C to 5.2 °C) warmer seasonally averaged LST within the urbanized territories than those of the surrounding landscapes. The magnitude of the urban LST anomaly corresponds to climates found 300–600 km to the South. In the climate change perspective, this magnitude corresponds to the expected regional warming by the middle or the end of the 21st century. Warmer urban climates, and specifically warmer upper soil layers, can support re-vegetation of the disturbed urban landscapes with more productive trees and tall shrubs. This afforestation is welcome by the migrant city population as it is more consistent with their traditional ecological knowledge. Survival of atypical, southern plant species encourages a number of initiatives and investment to introduce even broader spectrum of temperate blossoming trees and shrubs in urban landscapes. The unintended changes of the urban micro-climates in combination with knowledgeable urban planning could transform the Siberian pioneer settlements into places of belonging.</p></abstract><kwd-group xml:lang="en"><kwd>Surface urban heat island (SUHI)</kwd><kwd>traditional ecological knowledge (TEK)</kwd><kwd>urban green spaces</kwd><kwd>satellite data analysis</kwd><kwd>MODIS</kwd><kwd>NDVI</kwd><kwd>Siberia</kwd></kwd-group><funding-group><funding-statement xml:lang="en">Belmont Forum, Norwegian Research Council grant HIARC, Centre for Climate Dynamics grant</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">Archegova I.B. (2007). Thermal Regime of Tundra Soils under Reclamation and Restoration of Natural Vegetation, Eurasian Soil Science, Vol. 40, pp. 854–859.</mixed-citation><mixed-citation xml:lang="en">Archegova I.B. (2007). 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