云对地正闪前导脉冲的一些特性

D. Johari, V. Cooray, P. Hettiarachchi, M. Rahman, M. Ismail
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引用次数: 0

摘要

与负地闪相比,我们对正地闪的领导者的特征知之甚少。本文介绍了正面地闪前导传播过程中所观察到的电场脉冲的一些特性。我们详细分析了2014年瑞典乌普萨拉夏季雷暴期间50次正地闪产生的电场变化。在22%的病例中观察到明显的先导脉冲。它们在第一次击球前1.4毫秒或更短时间内出现。脉冲间隔时间为13.3 ~ 50.3 μs,平均值为24.7 μs。最大相对振幅为回冲程峰值的2.7 ~ 17.8%。观察到脉冲的发生与距离无关。相对振幅随距离的增加而减小。这些脉冲的存在表明引子以阶梯式的方式传播。还报道了一个案例,即在回击前出现负极性脉冲的正接地闪光。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Some characteristics of leader pulses in positive cloud-to-ground flashes
Compared to negative ground flashes, not much is known about the characteristics of leaders in positive ground flashes. This paper presents some characteristics of the electric field pulses observed during leader propagation in positive ground flashes. We analyzed in detail the electric field changes produced by 50 positive ground flashes during 2014 summer thunderstorms in Uppsala, Sweden. Pronounced leader pulses were observed in 22% of the cases. They were observed to occur 1.4 ms or less before the first return stroke. Interpulse duration ranged from 13.3 - 50.3 μs with a mean value of 24.7 μs. The largest relative amplitude ranged from 2.7 - 17.8 % of the return stroke peak. No dependence of the pulses occurrence were observed with distance. However, the relative amplitude were found to decrease with distance. The presence of these pulses suggests that the leaders propagate in a stepped manner. One case of positive ground flashes preceded by negative polarity pulses just before the return stroke is also reported.
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