摘要
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。
Based on the assumption that the bottom velocity is to be vanished, the density current in northwestern part of the East China Sea is calculated in this paper. The preliminary analysis of the results shows that the characteristics in the distribution of density current calculated is in good agreement with the marine conditions, i.e., the density current has annual change in strength with high value in summer and low value in winter, and spatial change in strength with higher value in external than in internal part, horizontally, and in upper than in lower layer, vertically.
出处
《海洋预报》
北大核心
1989年第2期31-36,共6页
Marine Forecasts
