东莞市雷电及雷灾特征综合分析
On Comprehensive Analysis of Lightning and Lightning Disaster Characteristics
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摘要: 利用5年闪电定位资料和14年雷电灾害资料,统计分析了东莞市闪电和雷灾情况,给出了东莞市闪电和雷灾的时空分布以及闪电电流特征.结果表明:东莞境内闪电主要为负闪,占97.6%,正闪的平均电流幅值(27.9 kA )略大于负闪的平均电流幅值(25.5 kA );平均每年发生雷灾30次,几乎每年都有人员伤亡,设备受损占80%,直接经济损失约100万元/年;闪电和雷灾的月变化均呈双峰特征(峰值出现在6月和8月),主要发生在汛期,但闪电发生频次与雷灾次数成反比;闪电和雷灾的日变化趋势基本一样,主要发生在午后,10:00-17:00闪电频数低于雷灾次数,其余时间则相反;闪电和雷灾空间分布与下垫面性质和环境有关,水乡片和沿海片闪电多雷灾少,城区片、埔田片和丘陵片闪电活动和雷灾基本一致,山区片闪电少雷灾多;另外根据闪电电流幅值和累积概率分布,得出了闪电电流幅值的集中区间以及所占比例的变化关系.Abstract: Lightning and lightning disaster around Dongguan have been analyzed according to the data of lightning location within five years and lightning disaster within fourteen years .The temporal ,spatial dis‐tribution and the current intensity characteristics of lightning and lightning disaster have been summarized under this analysis .The results show that the majority of lightning are negative account for 97 .6% with a mean intensity of 27 .9 kA ,which is slightly higher than that of positive lightning with a mean intensity of 25 .5 kA .The lighting disaster occurs 30 times on average with personnel casualties ,damages equipment (w hich is accounted for 80% )and direct economic loss of nearly one million every year .T he monthly chan‐ges of lightning and lightning disaster are characterized by bimodal distribution ,peak value appeared in June and August .Lightning frequency and lightning disaster mainly occurs in rainy season but in opposite direction .The diurnal variations of lightning and lightning disaster showed a similar trend and most of them occurred in the afternoon .The ratio of lightning frequency is less than lightning disaster from 10 :00 to 17 :00 ,other times is opposite .The spatial distribution of lightning and lightning disaster is closely re‐lated to the environment and the properties of underlying surface .Watery region and coastal region has more lightning activities than lightning disaster ,the opposite of mountain region .Lightning activities and lightning disaster have the same trend in city region ,field region and hills region .In addition ,according to the distributions of current intensity of lightning and accumulative probability of lightning current ,we got the concentrating range of current intensity and variations of ratio .
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