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在温跃层深度存在空间变化的条件下，建立约化重力热带海洋波致环流动力学模型。根据模型，热带海洋波致环流可看作是“广义地转运动”；波致子午向水体输运方程具有和Ｓｖｅｒｄｒｕｐ输运方程相似的形式；特别是波致环流对赤道准定常流系的“正负”贡献受制于温跃层深度的空间变化特征
Under the circumstance of spatial variation in the depth of the thermocline, a model of induced circulation of a reduced tropical ocean wave is established. According to the model, the tropical ocean wave induced circulation can be regarded as a “generalized geostrophic motion”; the wave-induced meridional water transport equation has a similar form to the Sverdrup transport equation; especially the wave-induced circulation has a positive effect on the “ Positive and negative ”contributions are subject to the spatial variation of the thermocline depth