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导言 我们曾提出了一种描述东中国海定常环流的全流模型,并用以对东中国海的冬季环流进行了数值模拟。该模型是以下列的风旋度—热盐梯度方程式来表述的:
Introduction We have presented a full-flow model describing the steady circulation in the East China Sea and used it to simulate the winter circulation in the East China Sea. The model is based on the following wind curl-hot salt gradient equation: