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An analytical study is made on the formation of the Cold Water Mass of the Yellow Sea (CWYS) and the relevant thermally driven circulation. The temperature and velocity field, obtained by solving the coupled equations of motion and heat conduction, show that, in summer, the CWYS has a horizontal cyclonic circulation (component) with vertical upwelling in the middle and downwelling at the edges, that the vertical convection (u-w components) occurs only within a thin layer near the thermocline. and that the deeper layer remains almost motionless. This current structure represents well the mechanisms responsible for the maintenance of the thermocline or CWYS during the wanner months. Comparisons between the theoretical and observed temperatures show very good qualitative and quantitative agreements for corresponding seasons.  相似文献   
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黄海冷水团热结构及其环流解析研究   总被引:10,自引:0,他引:10  
本文从一般的流体动力学-热力学方程组出发,通过对历史资料的分析,确立了描述黄海冷水团热结构及其环流的非线性控制方程组,得出近似解析解。理论计算结果表明,夏季北黄海冷水团区域存在中心上升边缘下降的气旋式密度环流。  相似文献   
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