Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms

In this study, the electric field signatures of negative ground flashes pertinent to the Swedish thunderstorms were recorded simultaneously during the summer of 2014 using wide (up to 100 MHz) and narrow (at 3 MHz and 30 MHz as central frequencies) bandwidth antenna systems. The electric field signa...

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Published in:Atmosphere
Main Author: Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
Format: Article
Language:English
Published: MDPI AG 2015
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-84953744486&doi=10.3390%2fatmos6121837&partnerID=40&md5=71492cd03d2b764124cee2d888d0885a
id 2-s2.0-84953744486
spelling 2-s2.0-84953744486
Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
2015
Atmosphere
6
12
10.3390/atmos6121837
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84953744486&doi=10.3390%2fatmos6121837&partnerID=40&md5=71492cd03d2b764124cee2d888d0885a
In this study, the electric field signatures of negative ground flashes pertinent to the Swedish thunderstorms were recorded simultaneously during the summer of 2014 using wide (up to 100 MHz) and narrow (at 3 MHz and 30 MHz as central frequencies) bandwidth antenna systems. The electric field signatures were recorded for a time duration of 250 ms. In the analysis, the whole flash was considered and a total of 98 flashes were chosen where electric field signatures of all wideband, 3 MHz and 30 MHz signals were present. It is observed that preliminary breakdown pulses are stronger radiators at 3 and 30 MHz compared to the return strokes. A comparison of our results with those of the previous studies obtained from different geographical regions clearly shows that the strength of preliminary breakdown pulses is higher in the temperate region (Sweden for instance) and is a function of latitude. © 2015 by the authors.
MDPI AG
20734433
English
Article
All Open Access; Gold Open Access; Green Open Access
author Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
spellingShingle Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
author_facet Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
author_sort Ismail M.M.; Rahman M.; Cooray V.; Sharma S.; Hettiarachchi P.; Johari D.
title Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
title_short Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
title_full Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
title_fullStr Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
title_full_unstemmed Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
title_sort Electric field signatures in wideband, 3 MHz and 30 MHz of negative ground flashes pertinent to Swedish thunderstorms
publishDate 2015
container_title Atmosphere
container_volume 6
container_issue 12
doi_str_mv 10.3390/atmos6121837
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-84953744486&doi=10.3390%2fatmos6121837&partnerID=40&md5=71492cd03d2b764124cee2d888d0885a
description In this study, the electric field signatures of negative ground flashes pertinent to the Swedish thunderstorms were recorded simultaneously during the summer of 2014 using wide (up to 100 MHz) and narrow (at 3 MHz and 30 MHz as central frequencies) bandwidth antenna systems. The electric field signatures were recorded for a time duration of 250 ms. In the analysis, the whole flash was considered and a total of 98 flashes were chosen where electric field signatures of all wideband, 3 MHz and 30 MHz signals were present. It is observed that preliminary breakdown pulses are stronger radiators at 3 and 30 MHz compared to the return strokes. A comparison of our results with those of the previous studies obtained from different geographical regions clearly shows that the strength of preliminary breakdown pulses is higher in the temperate region (Sweden for instance) and is a function of latitude. © 2015 by the authors.
publisher MDPI AG
issn 20734433
language English
format Article
accesstype All Open Access; Gold Open Access; Green Open Access
record_format scopus
collection Scopus
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