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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-3396</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>Морфология и деформация русла верхнего Амура</article-title><trans-title-group xml:lang="en"><trans-title>The Upper Amur channel morphology and deformations</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>Антроповский</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Antropovsky</surname><given-names>V. L.</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>Государственный гидрологический институт Росгидромета</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1997</year></pub-date><pub-date pub-type="epub"><day>24</day><month>11</month><year>2023</year></pub-date><volume>0</volume><issue>1</issue><fpage>45</fpage><lpage>53</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Антроповский В.И., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Антроповский В.И.</copyright-holder><copyright-holder xml:lang="en">Antropovsky V.l.</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/3396">https://geomorphology.igras.ru/jour/article/view/3396</self-uri><abstract><p>The paper presents morphometric and hydraulic characteristics, information on channel formations, character of ground and rate of deformation of the Upper Amur channel under natural conditions, some tentative estimates are given of the reservoir silting and general channel deformations downstream of the cascade of hydroengineering systems (downstream from the Novovoskresenovsky power station).</p></abstract><trans-abstract xml:lang="en"><p>The paper presents morphometric and hydraulic characteristics, information on channel formations, character of ground and rate of deformation of the Upper Amur channel under natural conditions, some tentative estimates are given of the reservoir silting and general channel deformations downstream of the cascade of hydroengineering systems (downstream from the Novovoskresenovsky power station).</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>
