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 .
季节性温跃层