Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area

ZHU Hai li

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Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area

- Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area
- Bulletin of Soiland Water Conservation Vol. 20, Issue 1, Pages: 39-41(2001)
- 作者机构：
  
  咸阳市气象局,陕西,咸阳,712000
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- Published：2001
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ZHU Hai li. Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area[J]. Bulletin of Soiland Water Conservation, 2001, 20(1): 39-41.
DOI：

ZHU Hai li. Circulation Characteristic of Rainstorm Inducing Landslide In Weibei Area[J]. Bulletin of Soiland Water Conservation, 2001, 20(1): 39-41. DOI：

摘要

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、高中低空天气系统的配置和相互作用以及环境条件和物理机制等方面探讨了其成因.

Abstract

The main studying objects were the rainstorms which had happened since 1980'5 and aroused landslide in Weibei area. the formation reasons of rainstorms were inquired in suitable disposition and interaction

environmental conditions and physical

chanism for weather systems of large

middle and small scales

at high

middle and low lati tucdes and altitudes.

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Keywords

references

郑秀雅，张廷治，等.东北暴雨[M].北京:气象出版，1992.102-104.

周全瑞，贺浩.暴雨数值预报方法研究[M].北京:气象出版社，1996.51-57.

汪之义.四川短期区域性暴雨专家系统[J].气象.1987(8):34-36.

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