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A Diagnostic Analysis of Heavy Rain in Mid-Tianshan Mountain

Zhou Li-wei

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Abstract

In this paper,the evolution of a heavy rain over the Mid-Tianshan Mountain of Xinjiang from 17:00 on 25 July to 08:00 on 26 July 2008 was analyzed by using the observations,T213 simulations,Fengyun-2C infrared images and Doppler radar echo.The result shows that the synoptic scale cold front cloud caused the heavy rain.The heavy rainfall center appeared in the southern of Southwest jet axis.The short-term heavy rainfall in each station was all resulted from mesoscale rain cluster of cold front rain cloud.

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What this paper is about

In this paper,the evolution of a heavy rain over the Mid-Tianshan Mountain of Xinjiang from 17:00 on 25 July to 08:00 on 26 July 2008 was analyzed by using the observations,T213 simulations,Fengyun-2C infrared images and Doppler radar echo.The result shows that the synoptic scale cold front cloud caused the heavy rain.The heavy rainfall center appeared in the southern of Southwest jet axis.The short-term heavy rainfall in each station was all resulted from mesoscale rain cluster of cold front rain cloud.

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Available abstract

In this paper,the evolution of a heavy rain over the Mid-Tianshan Mountain of Xinjiang from 17:00 on 25 July to 08:00 on 26 July 2008 was analyzed by using the observations,T213 simulations,Fengyun-2C infrared images and Doppler radar echo.The result shows that the synoptic scale cold front cloud caused the heavy rain.The heavy rainfall center appeared in the southern of Southwest jet axis.The short-term heavy rainfall in each station was all resulted from mesoscale rain cluster of cold front rain cloud.

Key concepts: Mesoscale meteorology, Cold front, Front (military), Climatology, Environmental science, Radar, Warm front, Meteorology

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