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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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1012</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>ГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>HYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSES</subject></subj-group></article-categories><title-group><article-title>Динамика профиля песчаного берега на различных масштабах времени</article-title><trans-title-group xml:lang="en"><trans-title>Shoreface profile dynamics in different time scales</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>Леонтьев</surname><given-names>И. О.</given-names></name><name name-style="western" xml:lang="en"><surname>Leont’yev</surname><given-names>I. O.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Москва</p></bio><email xlink:type="simple">igor.leontiev@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Институт океанологии им. П.П. Ширшова РАН</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2010</year></pub-date><pub-date pub-type="epub"><day>27</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><fpage>78</fpage><lpage>89</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Леонтьев И.О., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Леонтьев И.О.</copyright-holder><copyright-holder xml:lang="en">Leont’yev I.O.</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://hydrophysics.spbrc.ru/jour/article/view/1012">https://hydrophysics.spbrc.ru/jour/article/view/1012</self-uri><abstract><p>Динамика морского берега характеризуется как относительно кратковременными изменениями, так и долговременными тенденциями, проявляющимися на масштабах дсятков, сотен и тысяч лет. При прогнозе кратковременных штормовых деформаций наиболее успешными оказываются так называемые «модели процессов», имитирующие последовательность первичных механизмов, ответственных за транспорт наносов и формирование рельефа дна. Представленная модель CROSS-P применима к расчетам штормовых деформаций на песчаных берегах морей, озер и водохранилищ. Для анализа долговременной эволюции берега предложена модель SPELT, определяющая положение и форму профиля в зависимости от изменений уровня моря и дисбаланса бюджета наносов.</p></abstract><trans-abstract xml:lang="en"><p>Dynamics of the sea coast is characterized by both the short-term changes and the long-term trends manifested in the time scales of decades, centuries and milleniums. When modeling the short-term storm-induced deformations the process-based models turn out to be most successful as those simulate the suite of primary mechanisms responsible for sediment transport and bed deformations. Presented model CROSS-P is applicable to calculate the storm-induced deformations on sandy coasts of the seas, large lakes and water stores. To analyse the long-term coastal evolution the model SPELT is suggested determining the position and form of the profile depending on changes in sea level and imbalance of sediment budget.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>моделирование профиля берега</kwd><kwd>эрозия</kwd><kwd>аккумуляция</kwd><kwd>штормовые деформации</kwd><kwd>эволюция берега</kwd><kwd>бюджет наносов</kwd></kwd-group><kwd-group xml:lang="en"><kwd>coastal profile modeling</kwd><kwd>erosion</kwd><kwd>accumulation</kwd><kwd>storm-induced deformations</kwd><kwd>erosion</kwd><kwd>coastal evolution</kwd><kwd>sediment budget</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Леонтьев И.О. Прибрежная динамика: волны, течения, потоки наносов. 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