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dc.contributor.authorSato, Satoshi
dc.contributor.authorSimohira, Yasunao
dc.date.accessioned2020-02-06T10:57:21Z
dc.date.available2020-02-06T10:57:21Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/1834/16116
dc.description.abstractInternal tide was observed near Danzyo Gunto in Eastern China Sea The amplitude of temperature fluctuation of M2 tidal frequency was l℃ at 90 m depth where thermocline was situated. According to the vertical profile of temperature, it coincided with.the vertical motion whose amplitude was 10 m. If temperature fluctuation was caused by the first mode internal wave, the amplitude of horizontal current was 27 cm/sec at the surface layer. In its velocity field, we track the motions of fluid particles numerically. As a result, particles at the surface layer move more than 2 km over 1 cycle in the direction which the wave propagates. On the other hand, particles in the middle layer move in the opposite direction.en_US
dc.language.isojaen_US
dc.relation.urihttps://www1.kaiho.mlit.go.jp/GIJUTSUKOKUSAI/KENKYU/report/rhr24/rhr24-03.pdfen_US
dc.titleInternal tide near Danzyo Gunto in Eastern China Sea.en_US
dc.typeJournal Contributionen_US
dc.bibliographicCitation.issue24en_US
dc.bibliographicCitation.titleReport of Hydrographic and Oceanographic Researchesen_US
dc.description.statusPublisheden_US
dc.format.pagerangepp.45-58en_US
dc.type.refereedRefereeden_US
refterms.dateFOA2021-01-30T18:48:43Z


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