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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">10.59887/2073-6673.2023.16(4)-4</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1257</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>Моделирование баротропного прилива у юго-восточного побережья п-ва Камчатка с учетом точности глобальных приливных моделей в северо-западном регионе Тихого океана</article-title><trans-title-group xml:lang="en"><trans-title>Modeling of Barotropic Tide off the Southeastern Coast of the Kamchatka Peninsula in View of the Accuracy of Global Tidal Models in the Northwest Pacific Ocean</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0005-0374-486X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Романенков</surname><given-names>Д. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Romanenkov</surname><given-names>D. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>РОМАНЕНКОВ Дмитрий Анатольевич, кандидат географических наук</p><p>РИНЦ AuthorID: 61515</p><p>Scopus AuthorID: 6506855768,</p><p>WoS ResearcherID: U-8280-2017</p><p>117997, Нахимовский проспект, д. 36, Москва</p></bio><bio xml:lang="en"><p>36 Nakhimovsky Prosp., Moscow, 117997</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-9206-8253</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Софьина</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Sofina</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>СОФЬИНА Екатерина Владимировна, кандидат физико-математических наук</p><p>РИНЦ AuthorID: 169097</p><p>Scopus AuthorID: 23111468200,</p><p>WoS ResearcherID: E-3920–2014</p><p>117997, Нахимовский проспект, д. 36, Москва</p><p>192007, Воронежская улица, д. 79, Санкт-Петербург</p></bio><bio xml:lang="en"><p>36 Nakhimovsky Prosp., Moscow, 117997</p><p>79 Voronezhskaya Str., St. Petersburg, 192007</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Родикова</surname><given-names>А. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Rodikova</surname><given-names>A. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>РОДИКОВА Александра Евгеньевна</p><p>117997, Нахимовский проспект, д. 36, Москва</p></bio><bio xml:lang="en"><p>36 Nakhimovsky Prosp., Moscow, 117997</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><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН; Российский государственный гидрометеорологический университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences; Russian State Hydrometeorological University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>08</day><month>01</month><year>2024</year></pub-date><volume>16</volume><issue>4</issue><elocation-id>45–62</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Романенков Д.А., Софьина Е.В., Родикова А.Е., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Романенков Д.А., Софьина Е.В., Родикова А.Е.</copyright-holder><copyright-holder xml:lang="en">Romanenkov D.A., Sofina E.V., Rodikova A.E.</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/1257">https://hydrophysics.spbrc.ru/jour/article/view/1257</self-uri><abstract><p>В настоящей работе представлена реализация численной конечно-объемной региональной модели FESOM–С для предвычисления баротропной приливной динамики в тихоокеанских водах, прилегающих к юго-востоку п-ва Камчатка. Динамика воспроизводится для отдельных гармоник полусуточного M2 и суточного K1 диапазона приливного спектра, а также для суммарного прилива из 12-ти составляющих. Результаты расчетов, полученные на детальной неструктурированной сетке, интерпретируются в рамках волнового подхода. Региональная модель выявила изменчивость гармонических постоянных приливных колебаний уровня и характеристик течений на шельфе и изрезанном каньонами континентальном склоне из-за топографического рассеивания приливных волн. Оценены максимальные течения и вихревые структуры, связанные с остаточной приливной циркуляцией на шельфе и континентальном склоне. Выполнены эксперименты по чувствительности численного решения к заданию условий на открытых границах, взятых из двух современных глобальных приливных моделей FES2014 и TPXO9. Решение в региональной модели слабо зависит от этого выбора и хорошо согласуется с имеющимися немногочисленными данными по приливам. Однако оказалось, что решения самих глобальных моделей значимо отличаются между собой в поле приливных течений. Дополнительно было сделано сравнение точности решений глобальных приливных моделей для региона, включающего Охотское море и тихоокеанские воды вдоль островов Курильской гряды и п-ва Камчатка. Это сравнение было выполнено для верифицированной базы гармонических постоянных приливного уровня из советских и британских таблиц приливов. Хотя в среднем по области ошибки расчета приливного уровня малы и близки к официально заявленным, в отдельных районах региона ошибки глобальных моделей были весьма значимы. Их географическая привязка зависит от конкретной модели и сравниваемой приливной гармоники. Это означает, что к использованию результатов глобальных приливных моделей на региональном масштабе следует относиться с осторожностью, а актуальность развития регионального моделирования приливной динамики сохраняется.</p></abstract><trans-abstract xml:lang="en"><p>This study introduces the development and implementation of a regional numerical finite-volume model FESOM–C, specifically designed to accurately compute barotropic tidal dynamics in the Pacific waters adjacent to the southeastern region of the Kamchatka Peninsula. The dynamics of principal harmonics of the semidiurnal M2 and diurnal K1 tidal constituents are replicated, as well as the total tide, which encompasses 12 constituents. The computed results, obtained using a detailed unstructured grid, are interpreted through the Long-wave approach. The FESOM–C regional model revealed the variability of harmonic constants of tide and current characteristics within the shelf and canyon-cut continental slope, due to topographic scattering of tidal waves. The assessment includes the estimation of maximum currents and eddy structures associated with residual tidal circulation on the shelf and continental slope. To investigate the influence of varying open boundary conditions, sensitivity experiments have been conducted using data from two state-of-the-art global tidal models FES2014 and TPXO9. The findings reveal that the regional model’s solution exhibits only minimal dependency on this choice, and it aligns well with the limited available tidal data. Interestingly, the global models themselves demonstrate significant disparities in the tidal currents. Furthermore, we assess the accuracy of global tidal model solutions in a broader region encompassing the Sea of Okhotsk, as well as the Pacific waters along the Kuril Islands and the Kamchatka Peninsula. This assessment utilizes a verified database of tidal harmonic constants derived from the Soviet and British tide tables. While the average errors in tidal heights calculations remain minor and closely approximate officially declared values, certain areas within the region exhibit notable discrepancies in the outputs of the global models. These discrepancies are site-specific and vary depending on the particular model and tidal harmonic under consideration. This underscores the need for caution when applying results from global tidal models at the regional scale. Meanwhile, the importance of advancing regional tidal dynamics modeling remains evident.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>региональное моделирование</kwd><kwd>прилив</kwd><kwd>гармонические постоянные</kwd><kwd>остаточная циркуляция</kwd><kwd>завихренность</kwd><kwd>глобальные модели приливов</kwd><kwd>FES2014</kwd><kwd>TPXO9</kwd><kwd>модель FESOM–С</kwd><kwd>неструктурированная сетка</kwd><kwd>Охотское море</kwd><kwd>Курило-Камчатский регион</kwd><kwd>Авачинский залив</kwd></kwd-group><kwd-group xml:lang="en"><kwd>regional modeling</kwd><kwd>tide</kwd><kwd>harmonic constants</kwd><kwd>residual circulation</kwd><kwd>vorticity</kwd><kwd>global tide models</kwd><kwd>FES2014</kwd><kwd>TPXO9</kwd><kwd>FESOM–C model</kwd><kwd>unstructured grid</kwd><kwd>Sea of Okhotsk</kwd><kwd>Kuril-Kamchatka region</kwd><kwd>Avacha Bay</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено за счет гранта Российского научного фонда № 23-17-00174, https://rscf.ru/project/23-17-00174/.</funding-statement><funding-statement xml:lang="en">This work was supported by the Russian Science Foundation, project No. 23-17-00174, https://rscf.ru/en/project/23-17-00174/</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">Stammer D., Ray R.D., Andersen O.B. et al. 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