摘要
本文利用现场考察资料,分析了热带西太平洋低空大气温度层结基本特征。发现其边界层内往往有多个弱逆温层存在,在2000—3000m之间也常有弱逆温层存在。
In this paper, the main features of the low altitude atmospheric temperature stratification in the Western Tropical Pacific Ocean are analyzed based on the site observations.It is found from the analysis that there often exist several weak inversion layers in both the boundary layers and the altitude between 2000-3000m.
出处
《大气科学》
CSCD
北大核心
1991年第1期61-68,共8页
Chinese Journal of Atmospheric Sciences
关键词
热带
西太平洋
秋季
大气
温度
Several inversion layers
Vertical profile of temperature
Atmospheric temperature exploration
