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Dynamia Analysis of Rainstorm of Typhoon "KAEMI" by Means of Doppler Radar

LIU Xiao-di et al (Nanjing University of Information Science and Technology,Nanjing,Jiangsu 210044)  
With the observation data of Doppler Radar at Ganzhou,the dynamia of continuous heavy rain process were analyzed during Typhoon Kaemi having landed(July 25-26,2006).The results showed that the typhoon maintained a low-level jet during the whole process,which was the dynamia mechanism of rainstorm transmitted water vapor.Adverse wind regions(AWR),wind speed convergence, meso-and micro-scale cyclone and low-level convergence upper-level divergence all played an important role in rainstorm formation in part region of Ganzhou.
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