摘要
本文利用稠密的探空资料,分析了春季高原东侧的水平稳定层。确定了该稳定层的范围和强度,指出了其温度、湿度和流场特征,并初步探讨了其维持机制。
In this paper, the horizontal stable-layer, which occurred over the eastside of the Qinghai - Xizang Plateau in spring, is analysed with the dense radiosonde data. Its coverage and intensity are determined and the features of tem -perature, humidity and flow field are analysed. The mechanics are studied.
出处
《大气科学》
CSCD
北大核心
1991年第6期70-77,共8页
Chinese Journal of Atmospheric Sciences
基金
国家气象局高原基金与"长江中下游连阴雨
连晴天气研究"课题共同资助
关键词
大气
稳定层
流场
平流层
高原
Horizontal stable - layer
Quasistationary front
Differential advection
Continuous micro thermal, overcast and rainy weather during spring.
