Underlying Physical Mechanisms in Upward Positive Flashes

Fuente: arXiv
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Main Authors: Oregel-Chaumont, Toma, Šunjerga, Antonio, Kasparian, Jérôme, Rubinstein, Marcos, Rachidi, Farhad
Format: Preprint
Published: 2025
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author Oregel-Chaumont, Toma
Šunjerga, Antonio
Kasparian, Jérôme
Rubinstein, Marcos
Rachidi, Farhad
author_facet Oregel-Chaumont, Toma
Šunjerga, Antonio
Kasparian, Jérôme
Rubinstein, Marcos
Rachidi, Farhad
contents This study presents the first observation of a mixed mode 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 mixed mode 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 (ICC) 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.
format Preprint
id arxiv_https___arxiv_org_abs_2501_08110
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Underlying Physical Mechanisms in Upward Positive Flashes
Oregel-Chaumont, Toma
Šunjerga, Antonio
Kasparian, Jérôme
Rubinstein, Marcos
Rachidi, Farhad
Plasma Physics
Atmospheric and Oceanic Physics
Geophysics
This study presents the first observation of a mixed mode 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 mixed mode 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 (ICC) 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.
title Underlying Physical Mechanisms in Upward Positive Flashes
topic Plasma Physics
Atmospheric and Oceanic Physics
Geophysics
url https://arxiv.org/abs/2501.08110