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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(3)-5</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1237</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 функций распределения высот волн цунами вдоль восточного побережья острова Сахалин</article-title><trans-title-group xml:lang="en"><trans-title>Modeling of tsunami wave height distribution functions along the east coast of Sakhalin Island</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-1383-363X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Зайцев</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Zaytsev</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Андрей Иванович Зайцев</p><p>693023</p><p>ул. А.М. Горького, д. 25</p><p>Южно-Сахалинск</p><p>РИНЦ Author ID: 133746</p><p>Scopus Author ID: 36866694500</p><p>WoS Researcher ID: A-1772–2014</p></bio><bio xml:lang="en"><p>693023</p><p>Str. A.M. Gor’kogo, 25</p><p>Yuzhno-Sakhalinsk</p></bio><email xlink:type="simple">aizaytsev@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5092-0302</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Пелиновский</surname><given-names>Е. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Pelinovsky</surname><given-names>E. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ефим Наумович Пелиновский</p><p>603950</p><p>БОКС-120, ул. Ульянова, 46</p><p>603155</p><p>ул. Большая Печерская, 25/12</p><p>Нижний Новгород</p><p>РИНЦ Author ID: 103314</p><p>Scopus Author ID: 7004951110</p><p>WoS Researcher ID: I-3670–2013</p></bio><bio xml:lang="en"><p>603950</p><p>Box-120, Ulyanova Street, 46</p><p>603155</p><p>Str. Bolshaya Pecherskaya, 25/12</p><p>Nizhny Novgorod</p></bio><email xlink:type="simple">pelinovsky@ipfran.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Специальное конструкторское бюро средств автоматизации морских исследований ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Special Design Bureau for Marine Research Automation of RAS Far Eastern Branch</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Федеральное государственное бюджетное научное учреждение «Федеральный исследовательский центр Институт прикладной физики Российской академии наук»; Национальный исследовательский университет «Высшая школа экономики»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Applied Physics RAS; National Research University — Higher School of Economics</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>19</day><month>10</month><year>2023</year></pub-date><volume>16</volume><issue>3</issue><fpage>62</fpage><lpage>71</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Зайцев А.И., Пелиновский Е.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Зайцев А.И., Пелиновский Е.Н.</copyright-holder><copyright-holder xml:lang="en">Zaytsev A.I., Pelinovsky E.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://hydrophysics.spbrc.ru/jour/article/view/1237">https://hydrophysics.spbrc.ru/jour/article/view/1237</self-uri><abstract><p>   Изучаются функции распределение высот волн цунами вдоль восточного побережья острова Сахалин от источников, расположенных вдоль Курильских островов. Приводятся известные сведения о цунами на Сахалине. Многие из них моделировались численно, что позволяло оценить опасность волн цунами. В настоящей работе сделан упор на функциях распределения высот волн цунами, которые ранее вообще не рассчитывались для этого региона. С этой целью выполнены расчеты распространения волн цунами от гипотетических сильных землетрясений с М = 8,2, расположенных в районах Северных, Средних и Южных Курильских островов. Эти расчеты проведены с помощью вычислительного кода НАМИ-ДАНС, решающего нелинейные уравнения мелкой воды с использованием вложенных сеток с минимальным шагом около 9 м. Не имея достоверной прибрежной топографии, моделирование было выполнено до глубины около 3 м. Результаты расчетов подтвердили, что рассчитанные функции распределения высот волн цунами вдоль восточного побережья Сахалина хорошо аппроксимируются логнормальной функцией. Параметры этих распределений зависят от местоположения очага даже при одинаковых параметров землетрясения, что лишний раз подчеркивает существенную роль батиметрии морского дна на характеристики цунами на берегу.</p></abstract><trans-abstract xml:lang="en"><p>   The functions of the distribution of tsunami wave heights along the eastern coast of Sakhalin Island from sources located along the Kuril Islands are being studied. Known information about the tsunami on Sakhalin is given. Many of them were modeled numerically, which made it possible to assess the hazard of tsunami waves. The present work focuses on the functions of distributing the heights of tsunami waves, which were not previously calculated for this region at all. To this case, calculations were made of the propagation of tsunami waves from hypothetical strong earthquakes with M = 8.2 located in the regions of the Northern, Middle and Southern Kuril Islands. These calculations were carried out using the NAMI-DANCE computational code, which solves non-linear shallow water equations using nested grids with a minimum grid is about 9 m. Having no reliable coastal topography, the modeling was carried out to a depth of about 3 m. The results of the calculations confirmed that the calculated functions of the distribution of tsunami wave heights along the eastern coast of Sakhalin are well approximated by the lognormal function. The parameters of these distributions depend on the location of the source even with the same earthquake parameters, which once again emphasizes the significant role of seabed bathymetry on the characteristics of a tsunami on the shore.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>цунами</kwd><kwd>численное моделирование</kwd><kwd>логнормально распределение</kwd><kwd>Охотское море</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Tsunami</kwd><kwd>numerical modeling</kwd><kwd>lognormal distribution</kwd><kwd>Sea of Okhotsk</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа поддержана госзаданием СКБ САМИ ДВО РАН тема № 123012000050-6 (раздел «Краткая сводка исторических цунами, наблюдавшихся на восточном побережье острова Сахалин»), госзаданием ИПФ РАН тема № 0030-2021-0007 (раздел «Функции распределения высот волн»), и гранта РНФ № 23-27-00325 (разделы «Математическая модель распространения цунами» и «Результаты численных расчетов»)</funding-statement><funding-statement xml:lang="en">The work was supported by the state assignment of the SRB AMR FEB RAS topic No. 123012000050-6 (section “Brief summary of historical tsunamis observed on the eastern coast of Sakhalin Island”), the state assignment of the IAP RAS topic No. 0030-2021-0007 (section “Wave height distribution functions”), and the grant of the Russian National Research Fund No. 23-27-00325 (sections “Mathematical model of tsunami propagation” and “Results of numerical calculations”)</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">Го Ч.Н., Кайстренко В.М., Пелиновский Е.Н., Симонов К.В. 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