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dc.contributor.authorWatanabe, Shun-ichi
dc.contributor.authorUchida, Toru
dc.date.accessioned2019-09-12T12:48:47Z
dc.date.available2019-09-12T12:48:47Z
dc.date.issued2016
dc.identifier.urihttp://hdl.handle.net/1834/15522
dc.description.abstractCompiling thousands of vertical profiles of temperature and salinity measured during the seafloor geodetic observation, we statistically revealed the temporal stability in the depth of more than 1200 m within a few-miles-square region. We also found the spatial variations of temperature and salinity profiles. Specifically, temperature at 1200 m depth in the seafloor geodetic site ASZ 2(about 100 km southern off the Cape Ashizuri)is systematically higher than the other sites, which is strongly affected by the Kuroshio Current. On the other hand, at the seafloor geodetic site MYGI(about 100 km eastern off the Miyagi Prefecture), temporal intrusion of cold water was observed in the winter, reaching to the depth of about 800 m.en_US
dc.language.isojaen_US
dc.relation.urihttps://www1.kaiho.mlit.go.jp/GIJUTSUKOKUSAI/KENKYU/report/article.html#rhr53en_US
dc.titleStable structures of temperature and salinity validated by the repeated measurements in the few-miles-square regions off Japan coast in the western Pacific.en_US
dc.typeJournal Contributionen_US
dc.bibliographicCitation.issue53en_US
dc.bibliographicCitation.titleReport of Hydrographic and Oceanographic Researchesen_US
dc.description.statusPublisheden_US
dc.format.pagerangepp.57-81en_US
dc.type.refereedRefereeden_US
refterms.dateFOA2021-01-30T18:48:38Z


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