摘要
对奎玛流域一次冰雹天气的分析表明,在巴尔喀什湖低槽加强东移的环流背景下,低层水汽辐合、抬升启动和层结不稳定有利于该地区强对流的发生、发展,中尺度强对流云团的形成、发展是产生这次冰雹天气的主要原因。
The analysis on a hail process in the KuiMa river basin shows that under the circulation background which the tr ough in the Baerkashi Lake was strengthen ed and went east and the low -level moisture convergence ,lifting -up acti on and unstable stratification were good for the str ong convection occuring and develop ing in the area,the middle -scale con vective clouds came into being and developed was the main cause of the hail process.
出处
《新疆气象》
2002年第3期7-8,共2页
Bimonthly of Xinjiang Meteorology
