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彭双姿, 姚蓉, 刘从省, 田泽云, 林明丽, 刘红武, 陈静静, 尹忠海. 2010: “2010·05”湘中突发性强降水过程雷达回波特征分析. 暴雨灾害, 29(4): 69-75.
引用本文: 彭双姿, 姚蓉, 刘从省, 田泽云, 林明丽, 刘红武, 陈静静, 尹忠海. 2010: “2010·05”湘中突发性强降水过程雷达回波特征分析. 暴雨灾害, 29(4): 69-75.
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PENG Shuang-zi, YAO Rong, LIU Cong-sheng, TIAN Ze-yun, LIN Ming-li, LIU Hong-wu, CHENG Jing-jing, YIN Zhong-hai. 2010: Analysis of Radar Echo Characteristics of a Severe Rain Process in May of 2010 in Central Hunan. Torrential Rain and Disasters, 29(4): 69-75.
Citation: PENG Shuang-zi, YAO Rong, LIU Cong-sheng, TIAN Ze-yun, LIN Ming-li, LIU Hong-wu, CHENG Jing-jing, YIN Zhong-hai. 2010: Analysis of Radar Echo Characteristics of a Severe Rain Process in May of 2010 in Central Hunan. Torrential Rain and Disasters, 29(4): 69-75.
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“2010·05”湘中突发性强降水过程雷达回波特征分析

Analysis of Radar Echo Characteristics of a Severe Rain Process in May of 2010 in Central Hunan

    摘要
  • 摘要: 利用常规观测资料、自动站监测资料、多普勒雷达产品对2010年5月5日晚至6日湘中区域性强降水过程进行了分析。结果表明:暴雨发生前不稳定能量有一个加大的过程,K指数和沙氏指数在暴雨发生前有一定的指示意义,东南急流的建立与强降

     

    Abstract: By using the conventional observation data,automatic weather station observational data and radar echo data the regional severe rain occurred from May 5 to 6,2010 in the Central Hunan is analyzed.The results show

     

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