黔北一次低涡切变系统单多普勒雷达资料分析(英文)Doppler Radar Data Analysis of A Low-shear Vortex System in Northern Guizhou
李明元,张沪生
摘要(Abstract):
利用遵义CINRAD/CD多普勒雷达资料并结合其他资料分析了2008年7月10日发生在黔北地区的冰雹大风、短时强降水天气。结果表明,该系统是低涡切变带有冷空气南压过境影响所致;回波单体初期发展沿切变线排列,并在发展剧烈的回波所在处产生冰雹天气;降雹前出现最强回波60~65dBz,降雹时低仰角回波强度跃增到55~60dBz,回波高度11~15km,VIL值>35kg/m2;波分布有涡旋带状特征,当涡旋中心移向原有回波时,回波剧烈增强,产生持久深厚的辐合中气旋,地面出现冰雹大风;仁怀北部乡镇降雹和短时强降水可能与此区域左倒U型地形有关;湄潭永兴和鱼泉、仁怀学孔和喜头的回波是超级单体回波,其余各地降雹回波为多单体强回波。关键词低涡切变;多普勒雷达;回波特征
关键词(KeyWords): 低涡切变;多普勒雷达;回波特征
基金项目(Foundation):
作者(Author): 李明元,张沪生
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