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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-3057</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>Грядовой рельеф речного русла и его влияние на сезонные деформации перекатов</article-title><trans-title-group xml:lang="en"><trans-title>Ridge relief of the river channel and its impact on seasonal deformations of shallows</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>Турыкин</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Turykin</surname><given-names>L. A.</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>1993</year></pub-date><pub-date pub-type="epub"><day>02</day><month>02</month><year>2023</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>83</fpage><lpage>88</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Турыкин Л.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Турыкин Л.А.</copyright-holder><copyright-holder xml:lang="en">Turykin L.A.</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/3057">https://geomorphology.igras.ru/jour/article/view/3057</self-uri><abstract><p>Seasonal deformations of the shallows in the Chulym channel within the segment under study depend on the regime of movement of sandy and sandy-gravel ridges, the height of the ridges – 0.2 to 0.4 m - controls amplitudes of the shallows' crest fluctuations. Ridges of that order exist under velocities (averaged over the stream cross-section) from 0.4 m/s (the 1st threshold velocity) to 0.6 m/s (the 2nd threshold velocity).</p><p>The shallows are subdivided into three groups on the basis of average flow velocity (at different discharges) as related to the 2nd threshold velocity; the groups differ in the character of seasonal deformations of the channel.</p></abstract><trans-abstract xml:lang="en"><p>Seasonal deformations of the shallows in the Chulym channel within the segment under study depend on the regime of movement of sandy and sandy-gravel ridges, the height of the ridges – 0.2 to 0.4 m - controls amplitudes of the shallows' crest fluctuations. Ridges of that order exist under velocities (averaged over the stream cross-section) from 0.4 m/s (the 1st threshold velocity) to 0.6 m/s (the 2nd threshold velocity).</p><p>The shallows are subdivided into three groups on the basis of average flow velocity (at different discharges) as related to the 2nd threshold velocity; the groups differ in the character of seasonal deformations of the channel.</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>
