主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报

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一次鄂西地区暴雨过程中地形敏感性试验研究

姚昊; 潘晓滨;臧增亮   

  1. 解放军理工大学气象学院
  • 收稿日期:2008-06-27 修回日期:2008-07-29 出版日期:2008-10-01 发布日期:2008-10-01

Experiments on terrain sensitivity to a heavy rainstorm process in western Hubei province

YAO Hao; PAN Xiao-bin;ZANG Zeng-liang   

  1. Meteorological college, PLA University of Science and Technology
  • Received:2008-06-27 Revised:2008-07-29 Online:2008-10-01 Published:2008-10-01

摘要: 利用WRF模式中提供的不同平滑地形方案对2007年5月30-31日发生在湖北西部地区的暴雨过程进行数值模拟。在此基础上,利用WRF模式进行地形高度敏感性试验。结果表明:地形平滑方案与降水的时空分布有很大的相关性,地形越接近实际地形,降水的时空分布越接近实况;地形高度对降水的强度及落区影响较大,随着山脉地形高度的增加,迎风坡和背风坡的2个降水中心带有远离山脉的趋势,当山脉高度达到一定高度以后,迎风坡和背风坡的两个降水中心带又有靠近山脉的趋势。

关键词: 鄂西地区, 暴雨过程, WRF, 地形, 敏感性试验

Abstract: Based on the different terrain smooth schemes in the weather research and forecast (WRF) model, the numerical simulation of rainstorm process on May 30-31, 2007 in western Hubei province was carried through. And the sensitivity of terrain height was analyzed by WRF model. The results indicate that the terrain smooth schemes with the temporal and spatial distributions of precipitation are related. The closer the terrain is to the actual situation, the closer the temporal and spatial distributions of precipitation are to the actual situation. The terrain height can influence the intensity and falling area of precipitation. The two precipitation centers of windward slope and leeward slope tend to be far away from mountain with the terrain height increase of mountain, and they tend to be close to the mountain after the terrain height reaches the certain height.

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