A distinct negative leader propagation mode

Abstract The common phenomenon of lightning still harbors many secrets such as what are the conditions for lightning initiation and what is driving the discharge to propagate over several tens of kilometers through the atmosphere forming conducting ionized channels called leaders. Since lightning is...

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Autores principales: O. Scholten, B. M. Hare, J. Dwyer, N. Liu, C. Sterpka, I. Kolmašová, O. Santolík, R. Lán, L. Uhlíř, S. Buitink, A. Corstanje, H. Falcke, T. Huege, J. R. Hörandel, G. K. Krampah, P. Mitra, K. Mulrey, A. Nelles, H. Pandya, J. P. Rachen, T. N. G. Trinh, S. ter Veen, S. Thoudam, T. Winchen
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Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/cf9ed01604704320a54a252ce959fc83
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spelling oai:doaj.org-article:cf9ed01604704320a54a252ce959fc832021-12-02T15:08:23ZA distinct negative leader propagation mode10.1038/s41598-021-95433-52045-2322https://doaj.org/article/cf9ed01604704320a54a252ce959fc832021-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-95433-5https://doaj.org/toc/2045-2322Abstract The common phenomenon of lightning still harbors many secrets such as what are the conditions for lightning initiation and what is driving the discharge to propagate over several tens of kilometers through the atmosphere forming conducting ionized channels called leaders. Since lightning is an electric discharge phenomenon, there are positively and negatively charged leaders. In this work we report on measurements made with the LOFAR radio telescope, an instrument primarily build for radio-astronomy observations. It is observed that a negative leader rather suddenly changes, for a few milliseconds, into a mode where it radiates 100 times more VHF power than typical negative leaders after which it spawns a large number of more typical negative leaders. This mode occurs during the initial stage, soon after initiation, of all lightning flashes we have mapped (about 25). For some flashes this mode occurs also well after initiation and we show one case where it is triggered twice, some 100 ms apart. We postulate that this is indicative of a small (order of 5 km $$^2$$ 2 ) high charge pocket. Lightning thus appears to be initiated exclusively in the vicinity of such a small but dense charge pocket.O. ScholtenB. M. HareJ. DwyerN. LiuC. SterpkaI. KolmašováO. SantolíkR. LánL. UhlířS. BuitinkA. CorstanjeH. FalckeT. HuegeJ. R. HörandelG. K. KrampahP. MitraK. MulreyA. NellesH. PandyaJ. P. RachenT. N. G. TrinhS. ter VeenS. ThoudamT. WinchenNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
O. Scholten
B. M. Hare
J. Dwyer
N. Liu
C. Sterpka
I. Kolmašová
O. Santolík
R. Lán
L. Uhlíř
S. Buitink
A. Corstanje
H. Falcke
T. Huege
J. R. Hörandel
G. K. Krampah
P. Mitra
K. Mulrey
A. Nelles
H. Pandya
J. P. Rachen
T. N. G. Trinh
S. ter Veen
S. Thoudam
T. Winchen
A distinct negative leader propagation mode
description Abstract The common phenomenon of lightning still harbors many secrets such as what are the conditions for lightning initiation and what is driving the discharge to propagate over several tens of kilometers through the atmosphere forming conducting ionized channels called leaders. Since lightning is an electric discharge phenomenon, there are positively and negatively charged leaders. In this work we report on measurements made with the LOFAR radio telescope, an instrument primarily build for radio-astronomy observations. It is observed that a negative leader rather suddenly changes, for a few milliseconds, into a mode where it radiates 100 times more VHF power than typical negative leaders after which it spawns a large number of more typical negative leaders. This mode occurs during the initial stage, soon after initiation, of all lightning flashes we have mapped (about 25). For some flashes this mode occurs also well after initiation and we show one case where it is triggered twice, some 100 ms apart. We postulate that this is indicative of a small (order of 5 km $$^2$$ 2 ) high charge pocket. Lightning thus appears to be initiated exclusively in the vicinity of such a small but dense charge pocket.
format article
author O. Scholten
B. M. Hare
J. Dwyer
N. Liu
C. Sterpka
I. Kolmašová
O. Santolík
R. Lán
L. Uhlíř
S. Buitink
A. Corstanje
H. Falcke
T. Huege
J. R. Hörandel
G. K. Krampah
P. Mitra
K. Mulrey
A. Nelles
H. Pandya
J. P. Rachen
T. N. G. Trinh
S. ter Veen
S. Thoudam
T. Winchen
author_facet O. Scholten
B. M. Hare
J. Dwyer
N. Liu
C. Sterpka
I. Kolmašová
O. Santolík
R. Lán
L. Uhlíř
S. Buitink
A. Corstanje
H. Falcke
T. Huege
J. R. Hörandel
G. K. Krampah
P. Mitra
K. Mulrey
A. Nelles
H. Pandya
J. P. Rachen
T. N. G. Trinh
S. ter Veen
S. Thoudam
T. Winchen
author_sort O. Scholten
title A distinct negative leader propagation mode
title_short A distinct negative leader propagation mode
title_full A distinct negative leader propagation mode
title_fullStr A distinct negative leader propagation mode
title_full_unstemmed A distinct negative leader propagation mode
title_sort distinct negative leader propagation mode
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/cf9ed01604704320a54a252ce959fc83
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