诱发渭北滑坡暴雨的环流特征

Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area

以 2 0世纪 80年代以来发生在渭北地区的较强滑坡的暴雨为主要研究对象 ,从中小尺度、高中低纬度。

The main studying objects were the rainstorms which had happened since 1980s and aroused landslide in Weibei area. the formation reasons of rainstorms were inquired in suitable disposition and interaction, environmental conditions and physical mechanism for weather systems of large, middle and small scales, at high, middle and low latitudes and altitudes.