地闪与对流性天气系统中降水关系的分析

THE RELATIONSHIP BETWEEN CLOUD TO GROUND LIGHTNING AND PRECIPITATION IN THE CONVECTIVE WEATHER

  • 摘要: 利用1997年夏季在中国科学院兰州高原大气物理所平凉雷电与暴雹实验站设置的3站闪电定位系统所取得的地闪资料与雷达、降水及探空等资料进行了对比分析,发现地闪与对流性天气中的降水有较好的相关性,这种相关性用来对一般性对流天气中降水进行估测是可行的。通过非线性回归近似拟合得到平均雨强与对应时段内的地闪数回归方程为R=1.692lnF-0.273,相关系数r为0.8641.同时地闪频数与层结最大不稳定能量一样能够指示对流性天气的发生和发展。

     

    Abstract: Based on the obser vation data of the lightning location system(three direction finders are set at Liupan mountain,Peny ang and Pingliang lightning and thunderstorm experiment station respectively),radar,sounding and other weather background at Pingliang lightning and thunders to rmex periment station of Chinese Academy of Science between June and August in 1997,compared their applications in convective weather observation,it is found that cloud to ground lightning is an important index.The correlation coefficient between cloud to ground lightning and the precipitation in convective weatheris so high that cloud to ground lightning can estimate precipitation.The regression equation between the precipitation intensity (R) and the frequency of cloud to ground lightning(F)is R=1.692ln F-0.273,and the co rrelation coefficientris 0.8641.The frequency of cloud to ground lightning is just like the convective available potential energy,it can show the formation and development of the convective system.

     

/

返回文章
返回