通过对“中美热带西太平洋海-气联合考察”获得的大气温度探测资料分析,揭示了大气垂直对流旺盛的热带西太平洋暖水区低层大气普遍有逆温层存在的事实,并指出这些逆温层与信风逆温层和季风逆温层的显著区别是逆温层大多很弱、很薄,而且往往有多个逆温层同时存在。 Based on the analysis of the atmospheric temperature data obtained from the “Sino-US Tropical Western Pacific Ocean-Gas Exploration Survey”, it reveals the fact that there is a general inversion of the temperature in the lower atmosphere in the tropical western Pacific warm water zone with vertical convection. It is pointed out that these inverse The obvious difference between the temperature layer and the wind inversion layer and the monsoon inversion layer is that the inversion layer is mostly weak and thin, and often has multiple inversion layers simultaneously.