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地形对低涡大暴雨影响的数值模拟试验
引用本文:崔春光,房春花,胡伯威,王中.地形对低涡大暴雨影响的数值模拟试验[J].气象,2000,26(8):14-18.
作者姓名:崔春光  房春花  胡伯威  王中
作者单位:1. 武汉暴雨研究所,武汉,430074
2. 重庆市气象台
基金项目:中国气象局科技研究项目"三峡坝区降水暴雨天气预报方法的开发研究"资助.
摘    要:用MM5模式对1998年6月28 ̄29日长江三峡及其附近的低涡大暴雨过程作了初步的模拟研究。通过两种地表方案模拟的对比表明,四川盆地东侧山地对西南低涡的产生没有明显影响,但对这次低涡暴雨的强度及其分布有重要影响,主要表现在:涡前暖湿气流受大巴山-神农架山脉拦截形成迎风麓大暴雨带,鄂西南山区南坡也有迎风坡暴雨区,降水系统在东移过程中受盆地东侧整个山体阻滞迫使上游降水显著增强,下游降水系统在东移过程中

关 键 词:低涡  大暴雨  数值模拟  地形

Numerical Simulation of the Topographic Effects on Torrential Rain with South west China Vortex
Cui Chunguang,Fang Chunhua,Hu Bowei.Numerical Simulation of the Topographic Effects on Torrential Rain with South west China Vortex[J].Meteorological Monthly,2000,26(8):14-18.
Authors:Cui Chunguang  Fang Chunhua  Hu Bowei
Abstract:The torrential rain brought about by a South west China vortex in Changjiang Gorges and its vicinity in 28-29,June 1998 was simulated using MM5.Comparing the two simulations with different model topography schemes,it is indicated that the mountains in east Sichuan Basin has no significant effects on the genesis of South west China vortex,but has important influence on the intensity and the feature of distribution of the heavy rain events.Mainly, the warm and wet flow was blocked by Daba-Shenonggia mountain range and resulted in a torrential rain bend to the windward foot of the mountain range,which was also a heavy rain region at the windward slope of the southwest Hubei mountainous district,and the east moving precipitation system was detained by the mountains in east of the basin, as the sequence, the precipitation strengthened upstream and weakened downstream.
Keywords:vortex  torrential rain  numerical simulation
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