摘要
本文基于历史资料(1934～1988)和近期中、日黑潮合作调查结果分析指出,东海黑潮锋在其三维结构和季节变化等方面皆存在较明显的区域性差异.初步研究表明,地形效应是导致上述差异的主导因素.同时,季风和海面冷却在产生东海黑潮锋的区域性差异中亦起着重要的作用.
On the basis of the historical data(1934-1988)and the results of the PRC-Japan joint in- vestigation of the Kuroshio,analyses show that the Kuroshio front in the East China Sea has obvi- ous regional differences in its structure and seasonal variation.In a trial to explain theoretically these phenomena,topographic effect is considered to be the possible main factor for inducing the regional differences.Meanwhile,monsoon and the cooling of sea surface play a very important role in generating these differences.
出处
《黄渤海海洋》
CSCD
1992年第3期1-9,共9页
Journal of Oceanography of Huanghai & Bohai Seas
关键词
黑潮
潮锋
东海
区域性
差异
Kuroshio front
Regional
Differencef
