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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)-1</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1233</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>Микросейсмические колебания как индикатор тропических циклонов</article-title><trans-title-group xml:lang="en"><trans-title>Microseismic oscillations as an indicator of tropical cyclones</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5103-8138</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Чупин</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Chupin</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Владимир Александрович Чупин</p><p>690041</p><p>ул. Балтийская, 43</p><p>Приморский край</p><p>Владивосток</p><p>РИНЦ Author ID: 142439</p><p>Scopus Author ID: 7004931608</p><p>WoS Researcher ID: G-8803-2016</p></bio><bio xml:lang="en"><p>690041</p><p>Baltijskaya Street, 43</p><p>Vladivostok</p></bio><email xlink:type="simple">chupin@poi.dvo.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Тихоокеанский океанологический институт им. В.И. Ильичева ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch RAS</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>9</fpage><lpage>17</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чупин В.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Чупин В.А.</copyright-holder><copyright-holder xml:lang="en">Chupin V.A.</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/1233">https://hydrophysics.spbrc.ru/jour/article/view/1233</self-uri><abstract><p>   Представлены результаты регистрации микросейсмических колебаний в диапазоне частот инфразвуковых волн, выполненные в периоды активного влияния тропических циклонов на акваторию Японского моря. Данные получены береговым лазерно-интерференционным измерительным комплексом, состоящим из двухкоординатного лазерного деформографа и лазерного нанобарографа. На конкретном примере с использованием данных дистанционного зондирования показано слишком раннее прекращение сопровождения тайфуна мировыми метеорологическими агентствами при том, что циклон сохраняет свою вихревую структуру и энергетические характеристики. Показана динамика изменения характеристик инфразвуковых микросейсмических колебаний, которые зависят от траектории перемещения тайфунов и длительности их воздействия на акваторию моря. Приведены обобщенные результаты по некоторым группам тайфунов, имеющих похожие траектории перемещения, в результате чего максимальные амплитуды микросейсмических инфразвуковых колебаний проявляются на разных частотах. При прохождении в 2022 году тайфуна 5-й категории вблизи измерительного полигона был зарегистрирован микросейсмический сигнал, формирующийся при взаимодействии атмосферного вихря в тыловой части циклона с полем волн зыби. В результате регистрации наземными дистанционными методами определенных характеристик микросейсмических сигналов генерирующихся при прохождении тайфунов возможно использовать информацию для определения параметров перемещения тропических циклонов.</p></abstract><trans-abstract xml:lang="en"><p>   The paper presents the results of recording microseismic oscillations in the frequency range of infrasonic waves performed during the periods of active influence of tropical cyclones on the water area of the Sea of Japan. The data were obtained by a coastal laser-interference measuring complex consisting of a two-axis laser strainmeter and a laser nanobarograph. A case study using remote sensing data shows that the world meteorological agencies stopped tracking the typhoon too early, while the cyclone retains its vortex structure and energy characteristics. The dynamics of changes in the characteristics of infrasound microseismic oscillations, which depend on the trajectory of typhoons and the duration of their impact on the sea area, is shown. Generalised results are given for some groups of typhoons having similar trajectories of movement, as a result of which the maximum amplitudes of microseismic infrasonic oscillations are manifested at different frequencies. During the passage of a category 5 typhoon in 2022, a microseismic signal formed by the interaction of the atmospheric vortex in the rear part of the cyclone with the field of quicksand waves was registered near the measuring site. As a result of registration by ground-based remote sensing methods of certain characteristics of microseismic signals generated during the passage of typhoons, it is possible to use the information to determine the parameters of tropical cyclone movement.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>микросейсмические колебания</kwd><kwd>микросейсм</kwd><kwd>тропические циклоны</kwd><kwd>тайфуны</kwd><kwd>лазерный деформограф</kwd></kwd-group><kwd-group xml:lang="en"><kwd>microseismic oscillations</kwd><kwd>microseisms</kwd><kwd>tropical cyclones</kwd><kwd>typhoons</kwd><kwd>laser strainmeter</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках госбюджетных тем «Обоснование системы климатического мониторинга дальневосточных морей и разработка методов мониторинга экстремальных погодно-климатических явлений, связанных с океаном, на основе стационарных и мобильных измерительных комплексов, а также мультисенсорного спутникового зондирования» (№ 122122300025-8) (обработка и интерпретация данных) и «Изучение фундаментальных основ возникновения, развития, трансформации и взаимодействия гидроакустических, гидрофизических и геофизических полей Мирового океана» (№ АААА-А20-120021990003-3) (сопровождение измерительного комплекса)</funding-statement><funding-statement xml:lang="en">The work was supported in part by the State Assignments under Grant № 122122300025-8 «Justification of the system of climatic monitoring of the Far Eastern seas and development of methods for monitoring of extreme weather and climatic phenomena associated with the ocean, based on stationary and mobile measuring complexes, as well as multi-sensor satellite sensing» (data processing and interpretation) and “Investigation of fundamental bases of generation, development, transformation and interaction of hydroacoustic, hydrophysical and geophysical fields of the World Ocean” (AAAA-20-120021990003-3) (support of the measuring system</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">Долгих Г.И., Гусев Е.С., Чупин В.А. 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