Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms

All lightning strokes generate electromagnetic pulses –atmospherics– which can travel over distances of thousands of kilometers. Night-side atmospherics show typical frequency dispersion signatures caused by sub-ionospheric propagation. Their analysis can be used to determine the distance to the sou...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Santolík, O. (Ondřej), Kolmašová, I. (Ivana)
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
VLF
Online Access:https://doi.org/10.1038/s41598-017-13849-4
http://hdl.handle.net/11104/0275127
id ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0479115
record_format openpolar
spelling ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0479115 2024-02-04T10:02:26+01:00 Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms Santolík, O. (Ondřej) Kolmašová, I. (Ivana) 2017 https://doi.org/10.1038/s41598-017-13849-4 http://hdl.handle.net/11104/0275127 eng eng doi:10.1038/s41598-017-13849-4 urn:pissn: 2045-2322 urn:eissn: 2045-2322 http://hdl.handle.net/11104/0275127 info:eu-repo/semantics/openAccess lightning location VLF atmospherics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftczacademyscien https://doi.org/10.1038/s41598-017-13849-4 2024-01-09T17:39:53Z All lightning strokes generate electromagnetic pulses –atmospherics– which can travel over distances of thousands of kilometers. Night-side atmospherics show typical frequency dispersion signatures caused by sub-ionospheric propagation. Their analysis can be used to determine the distance to the source lightning, and therefore it represents a safe tool for investigation of distant thunderstorms, as well as for indirect observations of the lower ionosphere. However, such analysis has never been done on the dayside. Here we present the first results which show unusual daytime atmospherics with dispersion signatures originating from strong thunderstorms which occurred during winter months 2015 in the North Atlantic region. Using newly developed analysis techniques for 3-component electromagnetic measurements we are able to determine the source azimuth and to attribute these rare atmospherics to both positive and negative lightning strokes in northern Europe. We consistently find unusually large heights of the reflective ionospheric layer which are probably linked to low fluxes of solar X rays and which make the dayside subionospheric propagation possible. Although the atmospherics are linearly polarized, their dispersed parts exhibit left handed polarization, consistent with the anticipated continuous escape of the right-hand polarized power to the outer space in the form of whistlers. Article in Journal/Newspaper North Atlantic The Czech Academy of Sciences: Publication Activity (ASEP) Scientific Reports 7 1
institution Open Polar
collection The Czech Academy of Sciences: Publication Activity (ASEP)
op_collection_id ftczacademyscien
language English
topic lightning location
VLF
atmospherics
spellingShingle lightning location
VLF
atmospherics
Santolík, O. (Ondřej)
Kolmašová, I. (Ivana)
Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
topic_facet lightning location
VLF
atmospherics
description All lightning strokes generate electromagnetic pulses –atmospherics– which can travel over distances of thousands of kilometers. Night-side atmospherics show typical frequency dispersion signatures caused by sub-ionospheric propagation. Their analysis can be used to determine the distance to the source lightning, and therefore it represents a safe tool for investigation of distant thunderstorms, as well as for indirect observations of the lower ionosphere. However, such analysis has never been done on the dayside. Here we present the first results which show unusual daytime atmospherics with dispersion signatures originating from strong thunderstorms which occurred during winter months 2015 in the North Atlantic region. Using newly developed analysis techniques for 3-component electromagnetic measurements we are able to determine the source azimuth and to attribute these rare atmospherics to both positive and negative lightning strokes in northern Europe. We consistently find unusually large heights of the reflective ionospheric layer which are probably linked to low fluxes of solar X rays and which make the dayside subionospheric propagation possible. Although the atmospherics are linearly polarized, their dispersed parts exhibit left handed polarization, consistent with the anticipated continuous escape of the right-hand polarized power to the outer space in the form of whistlers.
format Article in Journal/Newspaper
author Santolík, O. (Ondřej)
Kolmašová, I. (Ivana)
author_facet Santolík, O. (Ondřej)
Kolmašová, I. (Ivana)
author_sort Santolík, O. (Ondřej)
title Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
title_short Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
title_full Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
title_fullStr Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
title_full_unstemmed Unusual Electromagnetic Signatures of European North Atlantic Winter Thunderstorms
title_sort unusual electromagnetic signatures of european north atlantic winter thunderstorms
publishDate 2017
url https://doi.org/10.1038/s41598-017-13849-4
http://hdl.handle.net/11104/0275127
genre North Atlantic
genre_facet North Atlantic
op_relation doi:10.1038/s41598-017-13849-4
urn:pissn: 2045-2322
urn:eissn: 2045-2322
http://hdl.handle.net/11104/0275127
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1038/s41598-017-13849-4
container_title Scientific Reports
container_volume 7
container_issue 1
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