雷暴天氣過程中降水結(jié)構(gòu)與閃電活動特征個例研究
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Characteristics of Precipitation Structure and Lightning Activities during a Thunderstorm Process
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    摘要:

    為深入分析四川雷暴天氣過程中降水和閃電活動特征,運(yùn)用統(tǒng)計與對比方法,對四川東南部一次雷暴過程中閃電活動及降水結(jié)構(gòu)之間的特征進(jìn)行研究。結(jié)果表明,強(qiáng)降水易發(fā)生在低層輻合,高層輻散的流場中,局部地區(qū)最大降水強(qiáng)度發(fā)生在2~5 km高度。降水開始1 h后,地閃頻數(shù)達(dá)到最高,地閃主要以負(fù)地閃為主,正地閃不活躍。對閃電活動與亮溫分布關(guān)系知,閃電活動主要發(fā)生在低于220 K降水云內(nèi),閃電活動發(fā)生的區(qū)域與降水落區(qū)一致。對總閃與地閃的分布知,負(fù)地閃主要分布在總閃的外圍。通過對四川雷暴過程的研究,對雷暴預(yù)報有一定的指導(dǎo)意義。

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    To better understood the characteristics of precipitation and lightning activities during a thunderstorms in Sichuan, by using the statistical and contrast methods, the features of the lightning activity and precipitation structure during a thunderstorm occurred in the southeastern Sichuan are analyzed. The results show that the heavy rainfall occurred in the flow field with low level convergence and upper level divergence, and the height of the local maximum precipitation zone located between 2 km and 5 km. After one hour of precipitation, the frequency of lightning flashes began to achieve the maximum, and the ground flashes were mainly negative CG (cloud to ground) flashes, and there were few positive CG flashes. According to the relationship between lightning activity and brightness temperature distribution, it is known that lightning activity occurs mainly in precipitation clouds with temperature being less than 220 K, and the areas of lightning activity are in agreement with precipitation areas. From the distribution of the total flashes and CG flashes, it can be known that negative CG flashes are distributed outside of the total flash area, and IC (intracloud) and CG flashes together impacted on the occurrence of lightning activities in the cloud system.The findings are useful to thunderstorm forecasting.

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蘇科學(xué),馮桂力,李波蘭.雷暴天氣過程中降水結(jié)構(gòu)與閃電活動特征個例研究[J].氣象科技,2014,42(5):865~873

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  • 收稿日期:2013-06-18
  • 定稿日期:2014-02-10
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  • 在線發(fā)布日期: 2014-10-30
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