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《Plateau Meteorology》 2006-03
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Impact of the Steep Terrain of Eastern Qinghai-Xizang Plateau on the Genesis and Development of Extreme Heavy Rainfall Event

LI Chuan, CHEN Jing,HE Guang-bi(Chengdu Institute of Plateau Meteorology,China Meteorological Administration,Chengdu 610072,China)  
Using the high resolotion mesoscale model analysis data,the impact of thecomplex mesoscale terrain on the east side of the Qinghai-Xizang Plateau to thegenesis and development of the heavy rainfall event was analyzed.The result shows that the dynamic blocking effect of the Qinghai-Xizang Plateau terrain on atmospheric circulationform the moisture transfer channel over the region of heavy rain scenario occurringand a strong vaporconvergence center in thenorthwest Sichuan and the upper reach of Yellow River.The terrain structure on the east side of Qinghai-Xizang Plateau and the accumulation of vaporin Sichuan Basin also form the high energy tongue and energy front in the lower layer and the potential instability energy in the lower troposphereof Sichuan Basin.The steep terrain on the east side of Qinghai-Xizang Plateau strengthens the ascendant motion.The strongest updraft movement occurredin the convergence area of the vertical shear of east and west wind and the steep landform,stimulating the release of theunsteady energy and rapid developmentof the strong convection.The process is also accompaniedby a mesoscale vortex on the east side of the Plateau.The most significant thermal and dynamical features is very different with mold rain with the high-temperature and high-humidity only appearing in the lower troposphereand strong vorticity column only appearing in the lower troposphere.
【Fund】: 四川省科技厅应用基础研究课题“四川五十年极端气候事件及未来趋势的研究”;; 国家自然科学基金项目(40475045);; 科技部社会公益研究专项(2004DIB3J119);; 四川省气象局重大项目“数值集合预报技术研究”资助
【CateGory Index】: P458.121
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