Baroclinic eddies south of Cheju Island in the East China Sea

Tetsuo Yanagi; Takanori Shimizu; Takeshi Matsuno

doi:10.1007/BF02239464

Baroclinic eddies south of Cheju Island in the East China Sea

Tetsuo Yanagi, Takanori Shimizu, Takeshi Matsuno

Division of Earth Environment Dynamics

Research output: Contribution to journal › Article › peer-review

22 Citations (Scopus)

Abstract

The detailed structures of baroclinic eddies, that is, an anticlockwise circulation in the upper layer and a clockwise one in the lower layer south of Cheju Island in the East China Sea have been revealed by intensive field observation. Such baroclinic eddies are accompanied by the southward spreading of the Yellow Sea Bottom Cold Water.

Original language	English
Pages (from-to)	763-769
Number of pages	7
Journal	Journal of Oceanography
Volume	52
Issue number	6
DOIs	https://doi.org/10.1007/BF02239464
Publication status	Published - Jan 1 1996

All Science Journal Classification (ASJC) codes

Oceanography

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10.1007/BF02239464

Cite this

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title = "Baroclinic eddies south of Cheju Island in the East China Sea",

abstract = "The detailed structures of baroclinic eddies, that is, an anticlockwise circulation in the upper layer and a clockwise one in the lower layer south of Cheju Island in the East China Sea have been revealed by intensive field observation. Such baroclinic eddies are accompanied by the southward spreading of the Yellow Sea Bottom Cold Water.",

author = "Tetsuo Yanagi and Takanori Shimizu and Takeshi Matsuno",

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AB - The detailed structures of baroclinic eddies, that is, an anticlockwise circulation in the upper layer and a clockwise one in the lower layer south of Cheju Island in the East China Sea have been revealed by intensive field observation. Such baroclinic eddies are accompanied by the southward spreading of the Yellow Sea Bottom Cold Water.

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Baroclinic eddies south of Cheju Island in the East China Sea

Abstract

All Science Journal Classification (ASJC) codes

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