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A theoretical model for the intrusion of the Kuroshio across the continental shelf of East China Sea 被引量:4
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作者 ZHANG QingHua QU YuanYuan +1 位作者 LI JianKe YIN XunQiang 《Science China Earth Sciences》 SCIE EI CAS CSCD 2015年第12期2289-2295,共7页
Here we use a two-layer model to study the dynamics of the intrusion of the Kuroshio onto the continental shelf. Results show that the interaction of the Kuroshio water and shelf water produces a stable upwelling zone... Here we use a two-layer model to study the dynamics of the intrusion of the Kuroshio onto the continental shelf. Results show that the interaction of the Kuroshio water and shelf water produces a stable upwelling zone above 100 m depth northeast of Talwan, which provides a dynamical explanation to the presence of the cold core previously observed by satellite. The affected shelf water from the interaction has an onshore portion, which turns right and becomes a northward alongshore flow when it moves closer to shore. This implies that the Kuroshio water cannot penetrate deep onto the inner part of the continental shelf, but it generates a strong northward jet that is formed mainly by the shelf water. 展开更多
关键词 KUROSHIO continental shelf UPWELLING alongshore flow STRATIFICATION
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