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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 pub-id-type="doi">10.59887/fpg/4pg1-agtu-u56k</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-677</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>Совместное моделирование ветровых волн  и волнового пограничного слоя</article-title><trans-title-group xml:lang="en"><trans-title>Coupled modelling of wind waves and wave boundary layer</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>Фокина</surname><given-names>К. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Fokina</surname><given-names>K. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Нахимовский пр., д. 36, Москва</p></bio><bio xml:lang="en"><p>117997, Nahimovskiy prospekt, 36, Moscow</p></bio><email xlink:type="simple">fokinakarina@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Булгаков</surname><given-names>К. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Bulgakov</surname><given-names>К. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Нахимовский пр., д. 36, Москва</p></bio><bio xml:lang="en"><p>117997, Nahimovskiy prospekt, 36, Moscow</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова, РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>01</day><month>04</month><year>2022</year></pub-date><volume>15</volume><issue>1</issue><fpage>73</fpage><lpage>81</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Фокина К.В., Булгаков К.Ю., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Фокина К.В., Булгаков К.Ю.</copyright-holder><copyright-holder xml:lang="en">Fokina K.V., Bulgakov К.Y.</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/677">https://hydrophysics.spbrc.ru/jour/article/view/677</self-uri><abstract><p>Сформулирована и реализована совместная модель волнового пограничного слоя и волн, объединяющая разработанные ранее соответствующие модели. Совместная модель использовалась в двух вариантах: с учетом и без учета волнового потока импульса. Проведены серии экспериментов с широким диапазоном изменения входных параметров (скорость ветра на верхней границе волнового пограничного слоя и обратный возраст волны) и рассчитаны значения метеорологических характеристик: скорости ветра, волнового и турбулентного потоков импульса в волновом пограничном слое. Полученные результаты проанализированы с целью продемонстрировать необходимость учета волнового потока импульса в моделях волнового пограничного слоя, а также показать особенности результатов совместного моделирования для описания волнового пограничного слоя. Показано, что результаты совместного моделирования для указанных метеорологических характеристик значительным образом отличаются от результатов, полученных по модели волнового пограничного слоя, для развитого и слаборазвитого волнения. Учет волнового потока импульса приводит к заметным отклонениям профиля скорости ветра в нижней части волнового пограничного слоя от логарифмического, применимого при описании атмосферного пограничного слоя.</p></abstract><trans-abstract xml:lang="en"><p>The coupled wind-wave model is considered. The model includes two components: the 1-D wave boundary layer model and the 2-D wave model. The coupled model is used in two versions: in the presence and the absence of the wave produced momentum flux. A series of experiments was performed for different external parameters: wind speed at the upper boundary of the wave boundary layer and the inverse wave age. The vertical profiles of wind velocity, turbulent and wave produced momentum fluxes were studied and compared to the results obtained from the wave boundary layer model. The comparison showed that the results of coupled modeling coincide exactly with the results from the wave boundary layer model in the case of fully developed waves and differ significantly if developing waves are considered. It is demonstrated that wave produced momentum flux produces considerable deviations of the wind velocity profile in the lower part of the wave boundary layer from the logarithmic profile.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>волновой пограничный слой</kwd><kwd>ветровые волны</kwd><kwd>волновой поток импульса</kwd><kwd>волновой спектр</kwd><kwd>взаимодействие океана и атмосферы</kwd></kwd-group><kwd-group xml:lang="en"><kwd>wave boundary layer</kwd><kwd>wind waves</kwd><kwd>wave produced momentum flux</kwd><kwd>wave spectrum</kwd><kwd>ocean-atmosphere interaction</kwd></kwd-group><funding-group><funding-statement xml:lang="en">Funding The presented results were obtained within the framework of the state program No FMWE-2021-0014</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">Зилитинкевич С.С. 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