%0 Journal Article
%T Basic characteristics of the rainstorm-producting mud-rock flow in Beijing area
北京泥石流暴雨基本特征
%A Wu Zhenghua
%A Chu Suolong
%A
吴正华
%A 储锁龙
%J 大气科学
%D 1992
%I
%X In this paper, temporal- spatial distribution of the rainstorm- producting mud- rock flow is analysed.It is pointed out that mud-rock flow rainstorm happens mainly in the situation of longitudinal circulation in North China. In the mud-rock flow area, local atmosphere is evidently latent instable, and the rainfall intensity is greater than mm/hour. The rainstorm area is located in the overlapping area of the mesoscale moist statical energe front zone, frontgenesis and strong moisture covergence on the surface.
%K Mud-rock flow
%K Rainstorm
%K Diagnostic analysis
%K Beijing
泥石流
%K 暴雨
%K 诊断分析
%K 北京
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=28A2F569B2458C17&jid=46874A5A102033D774D00D819E91CD68&aid=E7670AEE6C72A898&yid=F53A2717BDB04D52&vid=7801E6FC5AE9020C&iid=E158A972A605785F&sid=DA4893B5F9885621&eid=283B38DAD0D068F3&journal_id=1006-9895&journal_name=大气科学&referenced_num=2&reference_num=5