| A PRELIMINARY ANALYSIS ON THE CHARACTERISTICS OF THE KUROSHIO FRONTAL EDDY IN THE EAST CHINA SEA IN SPRING |
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| 作者姓名： | 郑义芳 黄卫民 Nakamura Yasuaki |
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| 作者单位： | First Institute of Oceanography，SOA，Qingdao 266003，First Institute of Oceanography，SOA，Qingdao 266003，Seikai Fisheries Research，JFA，Japan |
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| 摘 要： | The Kuroshi'o front eddy's surface and sectional isothermal distribution characteristics were analyzed on the basis of observation data obtained in April 13-16 of 1989 in the East China Sea. It was found from the similarity between these isothermal distributions with those in January and beginning of June for the years 1986-1990 that the Kuroshio front eddy often occurred from March to the beginning of June. The Kuroshio front eddy movement in the East China Sea in spring was along two routes: the Okinawa Trough route, and the continental shelf slope route. The two moving routes both in the surface layer and in the section are described, their causes are discussed, and differences are compared.
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| 收稿时间： | 5 June 1992 |
A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring |
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| Zheng Yifang,Huang Weimin,Nakamura Yasuaki.A PRELIMINARY ANALYSIS ON THE CHARACTERISTICS OF THE KUROSHIO FRONTAL EDDY IN THE EAST CHINA SEA IN SPRING[J].Chinese Journal of Oceanology and Limnology,1993,11(3):276-284. |
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| Authors: | Zheng Yifang Huang Weimin Nakamura Yasuaki |
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| Institution: | (1) First Institute of Oceanography, SOA, 266003 Qingdao;(2) Seikai Fisheries Research, JFA, Japan |
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| Abstract: | The Kuroshi'o front eddy's surface and sectional isothermal distribution characteristics were analyzed on the basis of observation data obtained in April 13-16 of 1989 in the East China Sea. It was found from the similarity between these isothermal distributions with those in January and beginning of June for the years 1986-1990 that the Kuroshio front eddy often occurred from March to the beginning of June. The Kuroshio front eddy movement in the East China Sea in spring was along two routes: the Okinawa Trough route, and the continental shelf slope route. The two moving routes both in the surface layer and in the section are described, their causes are discussed, and differences are compared. |
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| Keywords: | Kuroshio front eddy Kuroshio warm filament warm water eddy |
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