Multiphase turbulent flow explains lightning rings in volcanic plumes

Autores
Ichihara, Mie; Mininni, Pablo Daniel; Ravichandran, S.; Cimarelli, Corrado; Vagasky, Chris
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Hunga Tonga-Hunga Ha’apai (HTHH), a submarine caldera volcano of the Tonga archipelago, erupted explosively on January 15, 2022. The eruption generated the highest concentration of lightning events ever recorded, producing characteristic ring patterns of electrical discharges concentric to the vent. Here we reproduce the key features of the observations using three-dimensional simulations of buoyant plumes in a stably stratified atmosphere. Our idealized minimal model based on the Boussinesq approximation and heavy particles reveals that the essential mechanism underlying the formation of lightning rings is turbulence-induced particle clustering, which generates structures, favorable conditions for charge concentration by particle collision. We propose that the location, size, and persistence of lightning ring structures can reveal pulsatory activity at the vent that the opaque ash cloud hides from the satellite observation and can be used as a proxy for eruption parameters regulating the generation of hazardous impacts on the environment.
Fil: Ichihara, Mie. University of Tokyo; Japón
Fil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física del Plasma. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física del Plasma; Argentina
Fil: Ravichandran, S.. Indian Institute of Technology; India
Fil: Cimarelli, Corrado. Technische Universitat München; Alemania
Fil: Vagasky, Chris. No especifíca;
Materia
CLOUD PHYSICS
THUNDERSTORMS
VOLCANIC PLUMES
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/255850

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network_name_str CONICET Digital (CONICET)
spelling Multiphase turbulent flow explains lightning rings in volcanic plumesIchihara, MieMininni, Pablo DanielRavichandran, S.Cimarelli, CorradoVagasky, ChrisCLOUD PHYSICSTHUNDERSTORMSVOLCANIC PLUMEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Hunga Tonga-Hunga Ha’apai (HTHH), a submarine caldera volcano of the Tonga archipelago, erupted explosively on January 15, 2022. The eruption generated the highest concentration of lightning events ever recorded, producing characteristic ring patterns of electrical discharges concentric to the vent. Here we reproduce the key features of the observations using three-dimensional simulations of buoyant plumes in a stably stratified atmosphere. Our idealized minimal model based on the Boussinesq approximation and heavy particles reveals that the essential mechanism underlying the formation of lightning rings is turbulence-induced particle clustering, which generates structures, favorable conditions for charge concentration by particle collision. We propose that the location, size, and persistence of lightning ring structures can reveal pulsatory activity at the vent that the opaque ash cloud hides from the satellite observation and can be used as a proxy for eruption parameters regulating the generation of hazardous impacts on the environment.Fil: Ichihara, Mie. University of Tokyo; JapónFil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física del Plasma. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física del Plasma; ArgentinaFil: Ravichandran, S.. Indian Institute of Technology; IndiaFil: Cimarelli, Corrado. Technische Universitat München; AlemaniaFil: Vagasky, Chris. No especifíca;Springer2023-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/255850Ichihara, Mie; Mininni, Pablo Daniel; Ravichandran, S.; Cimarelli, Corrado; Vagasky, Chris; Multiphase turbulent flow explains lightning rings in volcanic plumes; Springer; Communications Earth & Environment; 4; 1; 11-2023; 1-122662-4435CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/s43247-023-01074-zinfo:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-023-01074-zinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:03:42Zoai:ri.conicet.gov.ar:11336/255850instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:03:42.463CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Multiphase turbulent flow explains lightning rings in volcanic plumes
title Multiphase turbulent flow explains lightning rings in volcanic plumes
spellingShingle Multiphase turbulent flow explains lightning rings in volcanic plumes
Ichihara, Mie
CLOUD PHYSICS
THUNDERSTORMS
VOLCANIC PLUMES
title_short Multiphase turbulent flow explains lightning rings in volcanic plumes
title_full Multiphase turbulent flow explains lightning rings in volcanic plumes
title_fullStr Multiphase turbulent flow explains lightning rings in volcanic plumes
title_full_unstemmed Multiphase turbulent flow explains lightning rings in volcanic plumes
title_sort Multiphase turbulent flow explains lightning rings in volcanic plumes
dc.creator.none.fl_str_mv Ichihara, Mie
Mininni, Pablo Daniel
Ravichandran, S.
Cimarelli, Corrado
Vagasky, Chris
author Ichihara, Mie
author_facet Ichihara, Mie
Mininni, Pablo Daniel
Ravichandran, S.
Cimarelli, Corrado
Vagasky, Chris
author_role author
author2 Mininni, Pablo Daniel
Ravichandran, S.
Cimarelli, Corrado
Vagasky, Chris
author2_role author
author
author
author
dc.subject.none.fl_str_mv CLOUD PHYSICS
THUNDERSTORMS
VOLCANIC PLUMES
topic CLOUD PHYSICS
THUNDERSTORMS
VOLCANIC PLUMES
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Hunga Tonga-Hunga Ha’apai (HTHH), a submarine caldera volcano of the Tonga archipelago, erupted explosively on January 15, 2022. The eruption generated the highest concentration of lightning events ever recorded, producing characteristic ring patterns of electrical discharges concentric to the vent. Here we reproduce the key features of the observations using three-dimensional simulations of buoyant plumes in a stably stratified atmosphere. Our idealized minimal model based on the Boussinesq approximation and heavy particles reveals that the essential mechanism underlying the formation of lightning rings is turbulence-induced particle clustering, which generates structures, favorable conditions for charge concentration by particle collision. We propose that the location, size, and persistence of lightning ring structures can reveal pulsatory activity at the vent that the opaque ash cloud hides from the satellite observation and can be used as a proxy for eruption parameters regulating the generation of hazardous impacts on the environment.
Fil: Ichihara, Mie. University of Tokyo; Japón
Fil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física del Plasma. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física del Plasma; Argentina
Fil: Ravichandran, S.. Indian Institute of Technology; India
Fil: Cimarelli, Corrado. Technische Universitat München; Alemania
Fil: Vagasky, Chris. No especifíca;
description Hunga Tonga-Hunga Ha’apai (HTHH), a submarine caldera volcano of the Tonga archipelago, erupted explosively on January 15, 2022. The eruption generated the highest concentration of lightning events ever recorded, producing characteristic ring patterns of electrical discharges concentric to the vent. Here we reproduce the key features of the observations using three-dimensional simulations of buoyant plumes in a stably stratified atmosphere. Our idealized minimal model based on the Boussinesq approximation and heavy particles reveals that the essential mechanism underlying the formation of lightning rings is turbulence-induced particle clustering, which generates structures, favorable conditions for charge concentration by particle collision. We propose that the location, size, and persistence of lightning ring structures can reveal pulsatory activity at the vent that the opaque ash cloud hides from the satellite observation and can be used as a proxy for eruption parameters regulating the generation of hazardous impacts on the environment.
publishDate 2023
dc.date.none.fl_str_mv 2023-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/255850
Ichihara, Mie; Mininni, Pablo Daniel; Ravichandran, S.; Cimarelli, Corrado; Vagasky, Chris; Multiphase turbulent flow explains lightning rings in volcanic plumes; Springer; Communications Earth & Environment; 4; 1; 11-2023; 1-12
2662-4435
CONICET Digital
CONICET
url http://hdl.handle.net/11336/255850
identifier_str_mv Ichihara, Mie; Mininni, Pablo Daniel; Ravichandran, S.; Cimarelli, Corrado; Vagasky, Chris; Multiphase turbulent flow explains lightning rings in volcanic plumes; Springer; Communications Earth & Environment; 4; 1; 11-2023; 1-12
2662-4435
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/s43247-023-01074-z
info:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-023-01074-z
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Springer
publisher.none.fl_str_mv Springer
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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