The intermediate and deep water formation in the Japan Sea
スポンサーリンク
概要
- 論文の詳細を見る
The intermediate and deep water formation process are studied by reproducing the past and present circulation numerically. The modeled past circulation shows that the bottom water formation takes place in the eastern Japan Basin, while the present state shows only the formation of intermediate water (the upper portion of the Japan Sea proper water (UJSPW)) which takes place mainly off VIadivostok. Besides the formation of the UJSPW, the formation process of the East Sea Intermediate Water (ESIW) characterized by salinity minimum is reproduced. The low salinity water at the surface advected from the north is subducted into the intermediate layer toward the east forming ESIW after meeting the East Korean Warm Current (EKWC) east of Korean coast of about 40ﾟN.
- 九州大学の論文
- 1999-12-30
著者
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Yoon J‐h
Kyushu Univ. Fukuoka Jpn
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Yoon Jong-hwan
Center For East Asian Ocean-atmosphere Research Research Institute For Applied Mechanics Kyushu Univ
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Yoon Jong-hwan
Research Institute For Applied Mechanics Kyushu University
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Yoon Jong-hwan
Dynamics Simulation Research Center Research Institute For Applied Mechanics Kyushu University
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Kawamura Hideyuki
Research Group For Environmental Science Nuclear Science And Engineering Directorate Japan Atomic En
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Kawamura Hideyuki
Graduate Student Research Institute For Applied Mechanics Kyushu University
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Kawamura Hideyuki
Research Group For Environmental Science Division Of Environment And Radiation Sciences Japan Atomic
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Kawamura Hideyuki
Research Group For Environmental Science Division Of Environment And Radiation Sciences Japan Atomic
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