Underlying mechanisms of transient luminous events: a review

Transient luminous events (TLEs) occasionally observed above a strong thunderstorm system have been the subject of a great deal of research during recent years. The main goal of this review is to introduce readers to recent theories of electrodynamics processes associated with TLEs. We examine t...

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Main Authors: V. V. Surkov, M. Hayakawa
Format: Article
Language:English
Published: Copernicus Publications 2012-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/30/1185/2012/angeo-30-1185-2012.pdf
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spelling doaj-e9f11de0773c48219989c9e78a876ee32020-11-24T21:10:52ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762012-08-01301185121210.5194/angeo-30-1185-2012Underlying mechanisms of transient luminous events: a reviewV. V. Surkov0M. Hayakawa1Moscow Engineering Physics Institute (MEPhI), Research Nuclear University of the Russian Federation, Moscow, RussiaAdvanced Wireless Communications Research Center, The University of Electro-Communications, Chofu Tokyo, JapanTransient luminous events (TLEs) occasionally observed above a strong thunderstorm system have been the subject of a great deal of research during recent years. The main goal of this review is to introduce readers to recent theories of electrodynamics processes associated with TLEs. We examine the simplest versions of these theories in order to make their physics as transparent as possible. The study is begun with the conventional mechanism for air breakdown at stratospheric and mesospheric altitudes. An electron impact ionization and dissociative attachment to neutrals are discussed. A streamer size and mobility of electrons as a function of altitude in the atmosphere are estimated on the basis of similarity law. An alternative mechanism of air breakdown, runaway electron mechanism, is discussed. In this section we focus on a runaway breakdown field, characteristic length to increase avalanche of runaway electrons and on the role played by fast seed electrons in generation of the runaway breakdown. An effect of thunderclouds charge distribution on initiation of blue jets and gigantic jets is examined. A model in which the blue jet is treated as upward-propagating positive leader with a streamer zone/corona on the top is discussed. Sprite models based on streamer-like mechanism of air breakdown in the presence of atmospheric conductivity are reviewed. To analyze conditions for sprite generation, thunderstorm electric field arising just after positive cloud-to-ground stroke is compared with the thresholds for propagation of positively/negatively charged streamers and with runway breakdown. Our own estimate of tendril's length at the bottom of sprite is obtained to demonstrate that the runaway breakdown can trigger the streamer formation. In conclusion we discuss physical mechanisms of VLF (very low frequency) and ELF (extremely low frequency) phenomena associated with sprites.https://www.ann-geophys.net/30/1185/2012/angeo-30-1185-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. V. Surkov
M. Hayakawa
spellingShingle V. V. Surkov
M. Hayakawa
Underlying mechanisms of transient luminous events: a review
Annales Geophysicae
author_facet V. V. Surkov
M. Hayakawa
author_sort V. V. Surkov
title Underlying mechanisms of transient luminous events: a review
title_short Underlying mechanisms of transient luminous events: a review
title_full Underlying mechanisms of transient luminous events: a review
title_fullStr Underlying mechanisms of transient luminous events: a review
title_full_unstemmed Underlying mechanisms of transient luminous events: a review
title_sort underlying mechanisms of transient luminous events: a review
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2012-08-01
description Transient luminous events (TLEs) occasionally observed above a strong thunderstorm system have been the subject of a great deal of research during recent years. The main goal of this review is to introduce readers to recent theories of electrodynamics processes associated with TLEs. We examine the simplest versions of these theories in order to make their physics as transparent as possible. The study is begun with the conventional mechanism for air breakdown at stratospheric and mesospheric altitudes. An electron impact ionization and dissociative attachment to neutrals are discussed. A streamer size and mobility of electrons as a function of altitude in the atmosphere are estimated on the basis of similarity law. An alternative mechanism of air breakdown, runaway electron mechanism, is discussed. In this section we focus on a runaway breakdown field, characteristic length to increase avalanche of runaway electrons and on the role played by fast seed electrons in generation of the runaway breakdown. An effect of thunderclouds charge distribution on initiation of blue jets and gigantic jets is examined. A model in which the blue jet is treated as upward-propagating positive leader with a streamer zone/corona on the top is discussed. Sprite models based on streamer-like mechanism of air breakdown in the presence of atmospheric conductivity are reviewed. To analyze conditions for sprite generation, thunderstorm electric field arising just after positive cloud-to-ground stroke is compared with the thresholds for propagation of positively/negatively charged streamers and with runway breakdown. Our own estimate of tendril's length at the bottom of sprite is obtained to demonstrate that the runaway breakdown can trigger the streamer formation. In conclusion we discuss physical mechanisms of VLF (very low frequency) and ELF (extremely low frequency) phenomena associated with sprites.
url https://www.ann-geophys.net/30/1185/2012/angeo-30-1185-2012.pdf
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