Underlying Physical Mechanisms in Upward Positive Flashes

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
T. Oregel-Chaumont, A. Šunjerga, J. Kasparian, M. Rubinstein, F. Rachidi
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引用次数: 0

Abstract

This study presents the first observation of a mixed mode (MM) of charge transfer during an upward positive flash, which was initiated from the Säntis Tower in Switzerland. High-speed camera footage, along with current and electric field measurements, revealed a downward-propagating recoil leader connecting to the grounded current-carrying plasma channel at a junction height of <1 km above the tip of the tower. This event triggered the “return stroke”-like main pulse associated with Type 1 upward positive flashes, leading us to propose a MM of charge transfer (normally observed in upward negative flashes) as the physical mechanism at play. Furthermore, the observed “Main pulse” shared characteristics with both mixed-mode and M-component-type initial continuous current pulses, challenging existing classification criteria, and supporting the notion of a unique mode of charge transfer with a range of junction length-dependent pulse characteristics, as opposed to two distinct modes. The recoil leader itself was accompanied by a sequence of fast electric field pulses indicative of step-like propagation, also an observational first. These findings contribute to improving our understanding of the mechanisms of charge transfer in upward lightning flashes.

Abstract Image

向上积极闪光的潜在物理机制
本研究首次观察到从瑞士Säntis塔发起的向上正闪中电荷转移的混合模式。高速摄像机镜头以及电流和电场测量显示,一个向下传播的后力引线连接到接地载流等离子体通道,连接高度在塔尖上方1公里处。这一事件触发了与1型向上的正闪相关的“回击”式主脉冲,导致我们提出一个MM的电荷转移(通常在向上的负闪中观察到)作为起作用的物理机制。此外,观察到的“主脉冲”具有混合模式和m分量型初始连续电流脉冲的共同特征,挑战了现有的分类标准,并支持具有一系列结长相关脉冲特性的独特电荷转移模式的概念,而不是两种不同的模式。反冲引子本身伴随着一系列快速电场脉冲,表明了阶梯式传播,这也是第一次观测到的。这些发现有助于提高我们对向上闪电中电荷转移机制的理解。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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