摘要
利用１９９４年４月６—７日发生在鄂、赣、皖交界地区的强风暴过程和８次历史个例，对其前一日资料作了温度平流和广义温度平流的计算分析。
The temperature advection and generalized temperature advection of the yesterday data for the severe storm processes in boundary region of Hubei,Jiangxi and Anhui provinces in April of 1994 and 8 other cases in history, are calculated and analysed.The results show that around the negative center of the difference between the upper and lower layers of generalized temperature advection will occure the severe convection weather.
出处
《高原气象》
CSCD
北大核心
1996年第3期363-369,共7页
Plateau Meteorology
关键词
广义温度平流
强对流天气
天气预报
Generalized temperature advection Severe convection weather
