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本文介绍了墨西哥湾流在流经乔治亚陆架时所产生的一种特殊的流动形态——锋面涡旋(frontal eddy)的特征及其模式,兼述黑潮在流经东海陆架时所观测到的类似现象。
This paper presents the characteristics and patterns of a special flow pattern of the Gulf Stream flowing through the Georgian shelf, the frontal eddy, and the patterns observed by the Kuroshio when it flows through the East China Sea shelf phenomenon.