Seasonal variation of the vertically averaged flow caused by the Jebar effect in the Tsushima Strait

研究成果: ジャーナルへの寄稿記事

7 引用 (Scopus)

抄録

The seasonal variation in the barotropic mode of motion caused by joint effect of the baroclinicity and bottom relief (Jebar effect) in the Tsushima Strait is investigated with the use of the diagnostic numerical model in this study. The Jebar effect in the Tsushima Strait is mainly caused by the intrusion of the Bottom Cold Water along the Korean coast in summer. This Jebar effect along the Korean coast locally supplies the negative vorticity in situ, and it forces the coastal current to be intensified. In summer, the volume transport of the Tsushima Warm Current entering the Tsushima Strait is biassed to the western part of the strait comparing with the flow pattern calculated in winter.

元の言語英語
ページ(範囲)617-633
ページ数17
ジャーナルJournal of Oceanography
50
発行部数6
DOI
出版物ステータス出版済み - 11 1 1994

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strait
seasonal variation
barotropic mode
volume transport
coastal current
coast
summer
cold water
vorticity
flow pattern
bottom water
relief
effect
winter

All Science Journal Classification (ASJC) codes

  • Oceanography

これを引用

Seasonal variation of the vertically averaged flow caused by the Jebar effect in the Tsushima Strait. / Isobe, Atsuhiko.

:: Journal of Oceanography, 巻 50, 番号 6, 01.11.1994, p. 617-633.

研究成果: ジャーナルへの寄稿記事

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