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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-996</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>ФУНДАМЕНТАЛЬНЫЕ ВОПРОСЫ ГИДРОФИЗИКИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>FUNDAMENTAL ISSUES OF HYDROPHYSICS</subject></subj-group></article-categories><title-group><article-title>Численное моделирование трехмерных потенциальных волн</article-title><trans-title-group xml:lang="en"><trans-title>Numerical Modeling of Three-Dimensional Potential Waves</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>Чаликов</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Chalikov</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург, Мельбурн</p></bio><email xlink:type="simple">dmitry-chalikov@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Санкт-Петербургский филиал Института океанологии им. П.П. Ширшова, РАН; Технологический университет Свинбурна</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2014</year></pub-date><pub-date pub-type="epub"><day>27</day><month>11</month><year>2022</year></pub-date><volume>7</volume><issue>1</issue><fpage>7</fpage><lpage>31</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чаликов Д.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Чаликов Д.В.</copyright-holder><copyright-holder xml:lang="en">Chalikov D.V.</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/996">https://hydrophysics.spbrc.ru/jour/article/view/996</self-uri><abstract><p>Разработана простая и точная схема, предназначенная для долговременного моделирования периодических трехмерных потенциальных волн. Схема основана на следующей поверхности неортогональной криволинейной системе координат. Потенциал скорости представлен как сумма аналитической и нелинейной компонент. Трехмерное уравнение для нелинейной компоненты решается итерациями. Используется Фурье-сеточный метод, аппроксимация второго порядка для вертикальных производных на растянутой сетке и схема Рунге—Кутта четвертого порядка для интегрирования по времени. Схема проверена воспроизведением бегущей волны Стокса. Однопроцессорная версия модели позволяет моделировать эволюцию волнового поля с сотнями тысяч степеней свободы в течение сотен периодов волны пика. Модель создана для исследования нелинейных свойств поверхностных волн, генерации экстремальных волн, прямых расчетов спектра нелинейных взаимодействий. После введения в модель схем расчета притока энергии и диссипации модель будет использоваться для прямого моделирования эволюции волнового поля.</p></abstract><trans-abstract xml:lang="en"><p>.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>трехмерные нелинейные поверхностные волны</kwd><kwd>волны Стокса</kwd><kwd>неустойчивость  Бенджамина—Фейера</kwd><kwd>нелинейные взаимодействия</kwd><kwd>интеграл Хассельманна</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Автор благодарит проф. А. С. Бабанина (Технологический университет Свинбурна, Мельбурн, Австралия) за поддержку и сотрудничество, а также анонимных рецензентов за высказанные замечания, позволившие внести много уточнений.  Работа поддержана грантом Российского фонда фундаментальных исследований № 11-05-0052</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Tolman H. L. 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