The southern core becomes one part of the warm eddy;
南侧的一个核心成为反气旋式涡旋的一部分。
The structure of mesoscale warm eddy was analyzed in order to verify this phenomenon. The necessity of shelf upwelling induced by mesoscale eddies was thus confirmed.
为证实这一现象，我们通过对中尺度暖涡流场结构分析，提出了中尺度暖涡诱导陆架上升流的必然性。
It is discovered, that sedimentary system have been controled by the Yellow Sea warm current and its derivative (cold eddy system).
经分析发现，这个沉积体系，完全受控于黄海暖流、冷涡及其相关的环流体系。
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