The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.
主要结果如下：海表风应力是影响温跃层的动力因子，对季节性温跃层的深度和强度均有重大影响，但对大洋温跃层的影响不大；
The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.
主要结果如下：海表风应力是影响温跃层的动力因子，对季节性温跃层的深度和强度均有重大影响，但对大洋温跃层的影响不大；
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