A theoretical model for the intrusion of the Kuroshio across the continental shelf of East China Sea
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 t...
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| Veröffentlicht in: | Science China. Earth sciences 2015-12, Vol.58 (12), p.2289-2295 |
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| container_title | Science China. Earth sciences |
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| creator | Zhang, QingHua Qu, YuanYuan Li, JianKe Yin, XunQiang |
| description | 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. |
| doi_str_mv | 10.1007/s11430-015-5130-6 |
| format | Article |
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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, QingHua</au><au>Qu, YuanYuan</au><au>Li, JianKe</au><au>Yin, XunQiang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A theoretical model for the intrusion of the Kuroshio across the continental shelf of East China Sea</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2015-12-01</date><risdate>2015</risdate><volume>58</volume><issue>12</issue><spage>2289</spage><epage>2295</epage><pages>2289-2295</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>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.</abstract><cop>Beijing</cop><pub>Science China Press</pub><doi>10.1007/s11430-015-5130-6</doi><tpages>7</tpages></addata></record> |
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| subjects | Boundary layer Continental shelves Earth and Environmental Science Earth Sciences Research Paper Upwelling Water depth Water resources management 上升流区 东海大陆架 两层模型 动力学解释 相互作用 陆架水 黑潮入侵 黑潮水 |
| title | A theoretical model for the intrusion of the Kuroshio across the continental shelf of East China Sea |
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