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Lightning mapping observation of a terrestrial gamma-ray flash

机译:地面伽玛射线闪光的闪电映射观察

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摘要

We report the observation with the North Alabama Lightning Mapping Array (LMA) related to a terrestrial gamma-ray flash (TGF) detected by RHESSI on 26 July 2008. The LMA data explicitly show the TGF was produced during the initial development of a compact intracloud (IC) lightning flash between a negative charge region centered at about 8.5 km above sea level (-22C temperature level) a higher positive region centered at 13 km, both confined to the convective core of an isolated storm in close proximity to the RHESSI footprint. After the occurrence of an LMA source with a high peak power (26 kW), the initial lightning evolution caused an unusually large IC current moment that became detectable 2 ms after the first LMA source and increased for another 2 ms, during which the burst of gamma-rays was produced. This slowly building current moment was most likely associated with the upward leader progression, which produced an uncommonly large IC charge moment change (+90 Ckm) in 3 ms while being punctuated by a sequence of fast discharge. These observations suggest that the leader development may be involved in the TGF production.
机译:我们报告了与RHESSI在2008年7月26日检测到的地面伽马射线闪光(TGF)有关的北阿拉巴马州闪电测绘阵列(LMA)的观测结果。LMA数据明确表明TGF是在紧凑型内部云的初始开发过程中产生的(IC)闪电在中心位于海拔约8.5 km(-22C温度水平)的负电荷区域与中心在13 km的较高正区域之间闪烁,两者均限于靠近RHESSI足迹的孤立风暴的对流核心。在出现具有高峰值功率(26 kW)的LMA源后,最初的雷电演变导致异常大的IC电流矩,该电流在第一个LMA源之后2 ms即可检测到,并持续了2 ms,在此期间突发产生了伽马射线。这种缓慢建立的电流极有可能与前导杆的上升有关,该电流在3 ms内产生了异常大的IC充电力矩变化(+90 Ckm),同时被一系列快速放电打断。这些观察结果表明,领导者的发展可能与TGF的产生有关。

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