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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-3493</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Процессы дельтообразования и возможности их математического моделирования</article-title><trans-title-group xml:lang="en"><trans-title>Delta formation processes and possibilities of their mathematical modeling</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>Михайлов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Mikhailov</surname><given-names>V. N.</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>19</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>3</fpage><lpage>15</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Михайлов В.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Михайлов В.Н.</copyright-holder><copyright-holder xml:lang="en">Mikhailov V.N.</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/3493">https://geomorphology.igras.ru/jour/article/view/3493</self-uri><abstract><p>Regularities of delta formation processes at river mouths are considered. Hydrological-morphological model of delta formation has been worked out. The model includes four units. The first unit considers process of sediment accumulation due to decrease of velocities in river flow, the second one deal with sediment balance at river mouth and the mouth cone formation. The third unit describes vertical changes of the channel within a delta; the fourth one describes interconnected processes of delta network dynamics and redistribution of water and sediment discharges between delta branches.</p></abstract><trans-abstract xml:lang="en"><p>Regularities of delta formation processes at river mouths are considered. Hydrological-morphological model of delta formation has been worked out. The model includes four units. The first unit considers process of sediment accumulation due to decrease of velocities in river flow, the second one deal with sediment balance at river mouth and the mouth cone formation. The third unit describes vertical changes of the channel within a delta; the fourth one describes interconnected processes of delta network dynamics and redistribution of water and sediment discharges between delta branches.</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>
