Chongqing Institute of Meteorological Sciences, Chongqing 401147, China
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History+
Received
2006-05-25
Issue Date
2007-06-28
Abstract
Through the statistically analyzing the typical atmospheric circulation and major effect systems of 31 regional rainstorm cases occurred in Chongqing,the major results can be summarized as:(1) the mountain torrential disasters in Chongqing mainly come from landslides,local mud-rock flow and flood in the brooks produced by the heavy precipitation;(2) the typical local storm mainly occurs from May to September,and the most cases happen in July;(3) befor the occurrence of the most rainstorm,the patterns of two ridges with one trough(occupying 52% in the total cases) or two troughs with one ridge(occupying 42% in the total cases) are located in the high latitude;(4) plateau trough(plateau shear),plateau eddy,subtropical high,southwest eddy,low-level jet and surface cold front,et al.,are the major effect systems.
WANG Zhong
, CHEN Yan-ying. , {{custom_author.name_en}}.
Analyses on Major Effect Systems and Typical Atmospheric Circulation Triggering Mountain Torrential Disasters in Chongqing. Plateau Meteorology. 2007, 26(3): 609-614