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dc.contributor.authorHusbjerg, Lasse Skaaning
dc.contributor.authorNeubert, Torsten
dc.contributor.authorChanrion, Olivier
dc.contributor.authorDimitriadou, Krystallia
dc.contributor.authorLi, Dongshuai
dc.contributor.authorStendel, Martin
dc.contributor.authorKaas, Eigil
dc.contributor.authorØstgaard, Nikolai
dc.contributor.authorReglero, Victor
dc.date.accessioned2023-04-04T07:32:07Z
dc.date.available2023-04-04T07:32:07Z
dc.date.created2022-09-26T09:44:27Z
dc.date.issued2022
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3061950
dc.description.abstractBlue electric streamer discharges in the upper reaches of thunderclouds are observed as flashes of 337.0 nm (blue) with faint or no emissions of 777.4 nm (red). Analyzing 3 years of measurements by the Atmosphere-Space Interactions Monitor on the International Space Station, we find that their distribution in rise time falls into two categories. One with fast rise times of 30 μs or less that are relatively unaffected by cloud scattering and emanate from within ∼2 km of the cloud tops, and another with longer rise times from deeper within the clouds. 50% of cells generating shallow events are associated with overshooting tops compared to 34% of cells generating deeper events. The median Convective Available Potential Energy of the cells is ∼70% higher for the shallow events and ∼38% higher for the deeper events than for lightning cells, suggesting the discharges are favored by strongly convective environments.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.titleObservations of Blue Corona Discharges in Thundercloudsen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.source.articlenumbere2022GL099064en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2022GL099064
dc.identifier.cristin2055254
dc.source.journalGeophysical Research Lettersen_US
dc.identifier.citationGeophysical Research Letters. 2022, 49 (12), e2022GL099064.en_US
dc.source.volume49en_US
dc.source.issue12en_US


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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