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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >The initial stage processes of rocket-and-wire triggered lightning as observed by VHF interferometry
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The initial stage processes of rocket-and-wire triggered lightning as observed by VHF interferometry

机译:通过VHF干涉仪观察到的火箭线触发闪电的初始过程

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We examine VHF interferometric images, channel-base currents, and broadband electric field waveforms of the initial stage (IS) in two rocket-and-wire triggered lightning flashes. Two types of negative leaders, termed "long-duration" and "short-duration" leaders, were imaged by the VHF interferometers during the IS of the two flashes. There were three leaders that had relatively long durations of more than a few milliseconds. These three leaders were not accompanied by a significant change of channel-base current during their early stages of development, indicating that they corresponded to intracloud (IC) discharges that were not connected to the grounded triggered-lightning channel. Two of these three leaders eventually connected to the triggered-lightning channel and initiated initial continuous current (ICC) pulses. The third long-duration leader apparently developed from the vicinity of an isolated negative charge region toward an upper-level positive charge region and toward a branch of the grounded channel; it served to bridge the positive charge region and the triggered-lightning channel, resulting in the opposite polarity portion of the bipolar ICC. The short-duration negative leaders had durations of some hundreds of microseconds. These negative leaders apparently recoiled along the conductive channels created by branches of the upward positive leader (UPL); they initiated ICC pulses when the grounded channel was sufficiently conductive. It follows that ICC pulses can be initiated either by recoil leaders or via interception of separate in-cloud leaders by a grounded current-carrying channel.
机译:我们在两个火箭和电线触发的闪电中检查了初始阶段(IS)的VHF干涉图图像,通道基电流和宽带电场波形。在两次闪光的IS期间,甚高频干涉仪对两种类型的负引导线(称为“长持续时间”和“短持续时间”引导线)进行了成像。三个领导者的持续时间相对较长,超过了几毫秒。这三位领导者在其发展的早期阶段并没有伴随着基极电流的显着变化,这表明它们对应于未连接到接地触发雷电通道的云内(IC)放电。这三个引导器中的两个最终连接到触发的雷电通道,并启动了初始连续电流(ICC)脉冲。第三长期领导者显然是从孤立的负电荷区附近向上层正电荷区以及接地通道的分支发展的。它起到桥接正电荷区和触发雷电通道的作用,从而形成双极性ICC的相反极性部分。短期负面领导者的持续时间约为数百微秒。这些消极的领导者显然沿着向上的积极领导者(UPL)的分支所创造的传导渠道反冲。当接地通道足够导电时,它们会启动ICC脉冲。因此,ICC脉冲可以由反冲前导器或通过接地的载流通道拦截单独的云中前导器来启动。

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