北黄海冷水团形成机制的初步探讨——Ⅱ.模式解的讨论

北黄海冷水团理论模式解揭示:冷水团的形成主要是北黄海洼地之上的过冬水体,由于入春以后海面不断增温,热量自表层向深层不断传递的结果.在冷水团成长期(6—7月),非线性垂直对流和平流效应不断增强,逐渐和由表及底增温的热扩散效应取得平衡,从而导致强温跃层和侧向锋面的形成.与此同时,三维热生密度环流相应而生;在冷水团整个成长期,水平密度环流始终呈气旋型的,而垂直环流则经历了由冷中心为下降流、边缘为上升流过渡到冷中心为上升流、边缘为下降流的两个阶段.     

北黄海冷水团形成机制的初步探讨——Ⅰ.模式解

本文建立反映北黄海冷水团及其密度环流形式机制和演变过程的流体动力学热力学方程组,通过某些物理假设,确定合理的数学物理模型,采用边界层理论分析和摄动分析技术,求得能阐述北黄海冷水团及其密度环流形成机制的温度和三维流速分布的近似解析解。     

STUDY ON THE FORMATIONAL MECHANISM OF THE NORTHERN YELLOW (HUANGHAI) SEA COLD WATER MASS(Ⅰ)——SOLUTION OF THE MODEL

A hydrodynamic-thermodynamic equation set was set up to reflect the formational mechanism and evolution of the Northern Yellow (Huanghai) Sea cold water mass (NYSCWM) and its density circulation. Appropriate mathematical physical models were established by using some physical postulations. An approximate analytic solution to expound the distributions of temperature and three-dimensional current velocity, which can be used to expound the formational mechanism of the NYSCWM and its density circulation is obtained by using the theory of boundary layer and perturbational analyses.     

STUDY ON THE FORMATIONAL MECHANISM OF THE NORTHERN YELLOW (Huanghai) SEA COLD WATER MASS (Ⅱ)——DISCUSSION ON THE SOLUTION OF THE MODEL

The theoretical solution of the model of the Northern Yellow (Huanghai) Sea Cold Water Mass (NYSCWM) reveals that the NYSCWM is mainly formed through the continuous temperature increase of the overwintered water body above the Northern Yellow Sea Depression (NYSD) after spring when heat is continuously conducted from the sea surface to the'deeper layer. In the NYSCWM's growing period, (June-July), nonlinear, vertical convection and advection effects continuously increase, and are gradually balanced by the heat diffusion effect as the temperature increases from the surface to the bottom, which leads to the formation of an intensive thermocline and lateral front. Meanwhile, the three-dimensional circulation correspondingly occurs. In the NYSCWM's entire growing period, the horizontal circulation is always in the cyclonic motion, while the vertical circulation passes through a transition from a period with the cold centre as downwelling to a period with the cold centre as upwelling.