Analyses on Major Effect Systems and Typical Atmospheric Circulation Triggering Mountain Torrential Disasters in Chongqing

WANG Zhong;CHEN Yan-ying

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Plateau Meteorology ›› 2007, Vol. 26 ›› Issue (3) : 609-614.

Analyses on Major Effect Systems and Typical Atmospheric Circulation Triggering Mountain Torrential Disasters in Chongqing

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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.

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Mountain torrent dis / Regional rainstorm / Atmosphere general c / Effect system

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WANG Zhong , CHEN Yan-ying. Analyses on Major Effect Systems and Typical Atmospheric Circulation Triggering Mountain Torrential Disasters in Chongqing. Plateau Meteorology. 2007, 26(3): 609-614

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