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本文较为详细地介绍了研究东海西北部密度流所采用的计算方法,并对计算结果作了初步的分析。分析的结果表明:该海域平均密度流速的变化有着夏强冬弱的特点;水平分布外侧大于内侧;垂直分布上层大于下层。
This paper introduces in more detail the calculation method used to study the density flow in the northwestern East China Sea, and makes a preliminary analysis of the calculation results. The results show that the change of the average density and velocity of the sea area is weak in summer and winter, the horizontal distribution is larger on the outside and the upper distribution is larger than the lower.