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dc.contributor.authorDimitriadou, Krystallia
dc.contributor.authorChanrion, Olivier
dc.contributor.authorNeubert, Torsten
dc.contributor.authorProtat, Alain
dc.contributor.authorLouf, Valentin
dc.contributor.authorHeumesser, Matthias
dc.contributor.authorHusbjerg, Lasse
dc.contributor.authorKöhn, Christoph
dc.contributor.authorØstgaard, Nikolai
dc.contributor.authorReglero, Victor
dc.date.accessioned2023-03-16T13:35:29Z
dc.date.available2023-03-16T13:35:29Z
dc.date.created2022-06-10T09:04:26Z
dc.date.issued2022
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3058839
dc.description.abstractWe report on observations of corona discharges at the uppermost region of clouds characterized by emissions in a blue band of nitrogen molecules at 337 nm, with little activity in the red band of lightning leaders at 777.4 nm. Past work suggests that they are generated in cloud tops reaching the tropopause and above. Here we explore their occurrence in two convective environments of the same storm: one is developing with clouds reaching above the tropopause, and one is collapsing with lower cloud tops. We focus on those discharges that form a distinct category with rise times below 20 μs, implying that they are at the very top of the clouds. The discharges are observed in both environments. The observations suggest that a range of storm environments may generate corona discharges and that they may be common in convective surges.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleAnalysis of Blue Corona Discharges at the Top of Tropical Thunderstorm Clouds in Different Phases of Convectionen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.source.articlenumbere2021GL095879en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2021GL095879
dc.identifier.cristin2030672
dc.source.journalGeophysical Research Lettersen_US
dc.identifier.citationGeophysical Research Letters. 2022, 49 (6), e2021GL095879.en_US
dc.source.volume49en_US
dc.source.issue6en_US


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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