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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-3142</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>Низкочастотные волновые движения и их связь с рельефом мелководий</article-title><trans-title-group xml:lang="en"><trans-title>Low frequency wave movements as related to the shallow seafloor relief</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>Ещенко</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Eshchenko</surname><given-names>L. 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>Шипилова</surname><given-names>Л. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Shipilova</surname><given-names>L. M.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В.Ломоносова, географический факультет</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1994</year></pub-date><pub-date pub-type="epub"><day>02</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>62</fpage><lpage>70</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ещенко Л.А., Шипилова Л.М., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Ещенко Л.А., Шипилова Л.М.</copyright-holder><copyright-holder xml:lang="en">Eshchenko L.A., Shipilova L.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://geomorphology.igras.ru/jour/article/view/3142">https://geomorphology.igras.ru/jour/article/view/3142</self-uri><abstract><p>To elucidate relief-forming role of long waves, fluctuations of wave levels were measured continuously throughout several days under conditions of both calm weather and all the phases of storm. The experiment was carried out in a very gently sloping nearshore zone and revealed the scale of wave motions to be about 1 km, which was in agreement with dimensions of most of constructional landforms on the sea floor. Another experiment was performed on a shallow far from the coast. The analysis of currents, temperature and salinity records suggested the water dynamics in the region to be under control of an anticyclonic vortex.</p></abstract><trans-abstract xml:lang="en"><p>To elucidate relief-forming role of long waves, fluctuations of wave levels were measured continuously throughout several days under conditions of both calm weather and all the phases of storm. The experiment was carried out in a very gently sloping nearshore zone and revealed the scale of wave motions to be about 1 km, which was in agreement with dimensions of most of constructional landforms on the sea floor. Another experiment was performed on a shallow far from the coast. The analysis of currents, temperature and salinity records suggested the water dynamics in the region to be under control of an anticyclonic vortex.</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>
