{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,12]],"date-time":"2025-10-12T02:18:37Z","timestamp":1760235517179,"version":"build-2065373602"},"reference-count":32,"publisher":"MDPI AG","issue":"17","license":[{"start":{"date-parts":[[2021,8,31]],"date-time":"2021-08-31T00:00:00Z","timestamp":1630368000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100012190","name":"Ministry of Science and Higher Education of the Russian Federation","doi-asserted-by":"publisher","award":["075-15-2020-776"],"award-info":[{"award-number":["075-15-2020-776"]}],"id":[{"id":"10.13039\/501100012190","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The article presents the results of microseismic signals of the \u201cvoice of the sea\u201d registration by a two-coordinate laser strainmeter during the passage of typhoons through and near the water area of the Sea of Japan. It was established that the \u201cvoice of the sea\u201d microseisms appear and disappear almost simultaneously with primary microseisms, i.e., the powerful \u201cvoice of the sea\u201d microseisms exist only in the presence of powerful wind waves, generated by a passing typhoon. According to the processing results of the obtained experimental data, the \u201cvoice of the sea\u201d microseisms generation area is located in the \u201csea-land\u201d transition zone, i.e., near and\/or in the surf zone. Based on the data of the two-coordinate laser strainmeter, we determined the bearing of the \u201cvoice of the sea\u201d microseisms generation area. The movement of this area coincides with the movement of the rear part of tropical cyclones.<\/jats:p>","DOI":"10.3390\/rs13173452","type":"journal-article","created":{"date-parts":[[2021,8,31]],"date-time":"2021-08-31T22:58:15Z","timestamp":1630450695000},"page":"3452","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":7,"title":["Cyclonic Process of the \u201cVoice of the Sea\u201d Microseism Generation and Its Remote Monitoring"],"prefix":"10.3390","volume":"13","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-2806-3834","authenticated-orcid":false,"given":"Grigory I.","family":"Dolgikh","sequence":"first","affiliation":[{"name":"V.I. Il\u2019ichev Pacific Oceanological Institute FEB RAS, 690041 Vladivostok, Russia"},{"name":"\u201cAEROCOSMOS\u201d Research Institute for Aerospace Monitoring, 105064 Moscow, Russia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5103-8138","authenticated-orcid":false,"given":"Vladimir A.","family":"Chupin","sequence":"additional","affiliation":[{"name":"V.I. Il\u2019ichev Pacific Oceanological Institute FEB RAS, 690041 Vladivostok, Russia"}]},{"given":"Egor S.","family":"Gusev","sequence":"additional","affiliation":[{"name":"V.I. Il\u2019ichev Pacific Oceanological Institute FEB RAS, 690041 Vladivostok, Russia"},{"name":"\u201cAEROCOSMOS\u201d Research Institute for Aerospace Monitoring, 105064 Moscow, Russia"}]},{"given":"Galina A.","family":"Timoshina","sequence":"additional","affiliation":[{"name":"\u201cAEROCOSMOS\u201d Research Institute for Aerospace Monitoring, 105064 Moscow, Russia"}]}],"member":"1968","published-online":{"date-parts":[[2021,8,31]]},"reference":[{"key":"ref_1","unstructured":"Bondur, V.G., and Krapivin, V.F. (2014). Space Monitoring of Tropical Cyclones, Scientific World."},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"871","DOI":"10.1134\/S0001433812090034","article-title":"Effect of mesoscale atmospheric vortex processes on the upper atmosphere and ionosphere of the Earth","volume":"48","author":"Bondur","year":"2012","journal-title":"Izv. Atmos. Ocean. 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