摘要
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。
The analyses of the sounding data of the atmosphere obtained from Sino-American joint air-sea interaction studies in the western tropical Pacific revealed that inversion layers occur within the lower atmospheric layer over the western tropical Pacific warm pool area where vertical convection of air prevails. The difference between the inversion layers of the low atmospheric layer and those of trade and monsoon showed that the former are generally weaker and thiner and several inversion layers often exist simultaneously.
出处
《海洋通报》
CAS
CSCD
北大核心
1993年第1期25-29,共5页
Marine Science Bulletin
关键词
热带
西太平洋
低层
大气
逆温层
western tropical Pacific
low atmosphpric layer
inversion layer
