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本文把海洋和大气边界层分为三层,利用地转动量近似的方法,考虑了大气的斜压性、层结和非线性效应,解析地给出了无限深海洋和大气边界层速度的垂直分布,并得出了在非线性情况下大气和海洋埃克曼抽吸速度,分析了它们与经典埃克曼解的差异性,揭示了海洋和大气相互作用的性质.同时,也得到了海面风和海面风应力的诊断关系.
In this paper, the ocean and atmosphere boundary layers are divided into three layers. Taking into account the atmospheric baroclinicity, stratification and nonlinear effects, the method of approximating the ground rotation is used to analyze the vertical distribution of the velocity of the infinite ocean and the atmospheric boundary layer Distribution and get the Ekman pumping speed of the atmosphere and ocean in the nonlinear case, analyzed the difference between them and the classical Ekman solution, revealed the nature of the interaction between the ocean and the atmosphere, and also obtained the sea surface Wind and sea surface wind stress diagnosis.