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本文引用两种一维模式对南黄海和东海的夏季跃层深度进行了诊断计算.解释了研究海区夏季温跃层深度分布特征的形成原因.证明在黄、东海陆架海区,潮混合对跃层深度具有重要作用.对中国近海沿岸某些所谓上升流现象提出了一种新的解释.
In this paper, two kinds of one-dimensional models are used to diagnose the summer thermocline depth in the South Yellow Sea and the East China Sea, and the reasons for the formation of the summer thermocline depth distribution are explained. It is proved that in the Yellow Sea and East China Sea, Depth has an important role to put forward a new explanation for some of the so-called upwelling phenomena in China’s coastal areas.