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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Unusual lightning electric field waveforms observed in Kathmandu, Nepal, and Uppsala, Sweden
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Unusual lightning electric field waveforms observed in Kathmandu, Nepal, and Uppsala, Sweden

机译:在加德满都,尼泊尔和瑞典乌普萨拉观察到不寻常的闪电电场波形

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AbstractUnusual lightning events have been observed in Uppsala, Sweden, and Kathmandu, Nepal, using essentially the same electric field measuring system developed at Uppsala University. They occurred in the storms that also generated “normal” lightning events. The unusual events recorded in Uppsala occurred on one thunderstorm day. Similar events were observed in Kathmandu on multiple thunderstorm days. The unusual events were analyzed in this study assuming them to be positive ground flashes (+CGs), although we cannot rule out the possibility that some or most of them were actually cloud discharges (ICs). The unusual events were each characterized by a relatively slow, negative (atmospheric electricity sign convention) electric field waveform preceded by a pronounced opposite-polarity pulse whose duration was some tens of microseconds. To the best of our knowledge, such unusual events have not been reported in the literature. The average amplitudes of the opposite-polarity pulses with respect to those of the following main waveform were found to be about 33% in Uppsala (N?=?31) and about 38% in Kathmandu (N?=?327). The average durations of the main waveform and the preceding opposite-polarity pulse in Uppsala were 8.24?ms and 57.1?μs, respectively, and their counterparts in Kathmandu were 421 μs and 39.7?μs. Electric field waveforms characteristic of negative ground flashes (-CGs) were also observed, and none of them exhibited an opposite-polarity pulse prior to the main waveform. Possible origins of the unusual field waveforms are discussed.
机译:<![CDATA [ 抽象 在乌普萨拉,瑞典和加德满都,尼泊尔,使用基本相同的电场测量,观察到了不寻常的闪电事件系统在乌普萨拉大学开发。它们发生在风暴中,这些风暴也产生了“正常”闪电事件。在乌普萨拉录制的不寻常事件发生在一个雷暴日。在多个雷暴日内在加德满都观察了类似的事件。在本研究中分析了不寻常的事件,假设它们是积极的闪烁(+ CG),尽管我们不能排除一些或大多数人实际上是云放电(ICS)的可能性。各种事件各自为特征在于相对较慢的负(大气电符号序列)电场波形,其前面以发音相反极性脉冲,其持续时间为一些数十秒的微秒。据我们所知,这些不寻常的事件尚未在文献中报告。相对于以下主要波形的相对极性脉冲的平均幅度被发现为乌普萨拉(n?= 31)的约33%,在加德满都(n?= 327)中约38%。乌普萨拉的主波形和前面的相对极性脉冲的平均持续时间分别为8.24℃,分别为57.1?μs,在加德满都的同行分别为421μs和39.7?μs。还观察到负接地闪光(-CG)的电场波形,并且它们在主波形之前,它们都没有表现出相反的极性脉冲。讨论了不寻常的场波形的可能起源。

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