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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">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-3473</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Особенности развития тундрового микрорельефа Таймыра</article-title><trans-title-group xml:lang="en"><trans-title>Characteristics of tundra microrelief development at the Taimyr</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>Романенко</surname><given-names>Ф. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Romanenko</surname><given-names>F. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Холинов</surname><given-names>А. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Kholnov</surname><given-names>A. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Зарецкая</surname><given-names>Н. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Zaretskaya</surname><given-names>N. E.</given-names></name></name-alternatives><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, географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1998</year></pub-date><pub-date pub-type="epub"><day>14</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>1</issue><fpage>100</fpage><lpage>107</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Романенко Ф.А., Холинов А.П., Зарецкая Н.Е., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Романенко Ф.А., Холинов А.П., Зарецкая Н.Е.</copyright-holder><copyright-holder xml:lang="en">Romanenko F.A., Kholnov A.P., Zaretskaya N.E.</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://geomorphology.igras.ru/jour/article/view/3473">https://geomorphology.igras.ru/jour/article/view/3473</self-uri><abstract><p>Results of ten years field researches in tundra regions of Taimyr and West Siberia are presented. Field experiments, modeling of spots' formation, mapping of cryogenic microrelief, were fulfilled. The main causes of central bald spot formation are the lack of nutrient stuff washed away down the soil profile and the excessive iciness in the near-surface soil. The main factors of this process - ground temperature zero crossing, snowmelt, freezing-thawing of the near surface ground. The peculiarities of formation and development of different types of microrelief have zonal character and depend on humidification of surface.</p><p> </p></abstract><trans-abstract xml:lang="en"><p>Results of ten years field researches in tundra regions of Taimyr and West Siberia are presented. Field experiments, modeling of spots' formation, mapping of cryogenic microrelief, were fulfilled. The main causes of central bald spot formation are the lack of nutrient stuff washed away down the soil profile and the excessive iciness in the near-surface soil. The main factors of this process - ground temperature zero crossing, snowmelt, freezing-thawing of the near surface ground. The peculiarities of formation and development of different types of microrelief have zonal character and depend on humidification of surface.</p><p> </p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
