摘要
对比分析指出,江南岭北地区呈准静止的、坡度近似为1/230、低空有强偏南风伴随的低空比湿锋区是该地区3月份发生连阴雨的湿度条件。该地区的逆湿层可能与上述比湿锋区有关。
Based on comparison and analysis, it is shown that there is a quasi-static specific humidity front with a slope of. 1/230 and accompanied by a stronger southerly wind in the lower layer during the continuously rainy March in the areas south to the Changjiang River and north to the Five Ridges. The humidity inversion in the lower layer may be related to the specific humidity front over the areas.
出处
《气象》
CSCD
北大核心
1989年第10期36-43,共8页
Meteorological Monthly
基金
"长江中下游连阴雨
连晴天研究"课题
