昆明市2次区域性强降水过程对比分析

Contrast analysis of two heavy rainfall cases in Kunming

  • 摘要: 利用NCEP1°×1°再分析资料和卫星资料从降水情况、天气系统、水汽条件和垂直运动等方面,对2014年6月出现在昆明市的2次区域性强降水过程进行对比分析,结果表明:2次过程均由冷锋切变线南下而引起,在水汽输送和垂直运动等方面均存在有利条件.前一次过程在500 hPa上有高空槽配合,后一次过程在500 hPa上存在两高间的辐合区,且水汽辐合和上升运动等明显强于前一次过程,因此在各种有利条件的配合下,后一次区域性降水明显强于前一次过程.

     

    Abstract: Based on the NCEP1°×1° reanalysis data and satellite data,the contrast analysis of two heavy rainfall cases in Kunming is performed with rainfall,weather station,water vapor and vertical motion.The results show that the two processes were influenced by Chuan-Dian shear line,and there are some favorable conditions in the water vapor transportation and vertical motion.In the former process there is a high-level trough in 500 hPa.In the latter process there is a convergence between two hights in 500 hPa,and water vapor convergence and ascending motion are stronger than the former process,therefore supported by all kinds of favorable conditions,the rainfall in the latter process is stronger than the former process.

     

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