摘要
对哈密2001年10月大降水天气过程的降水成因进行了分析,表明低空急流和上升运动是其形成的重要机制,同时在哈密地区大降水天气短期预报着眼点方面获得了一些有益的启示。
This paper analysed the contributin g factor of a heavy rainfall process i n October of 2001.It has been shown th at the low -level Jet and asceding motio n were the important mechanism of the heavy rainfall process.Some useful conclusions on short -term forcast of hervy rainf ul in Hami area is obtained.
出处
《新疆气象》
2003年第3期13-15,共3页
Bimonthly of Xinjiang Meteorology
