Thus, there exist some relationship between the multi-eddy structure of the South China Sea circulation and mesoscale fluctuation.
因此，南海环流的多涡结构与中尺度波动之间存在着一定的联系。
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。
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