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dc.contributor.authorSoler, S.
dc.contributor.authorGordillo-Vázquez, F.J.
dc.contributor.authorPérez-Invernón, F.J.
dc.contributor.authorLuque, A.
dc.contributor.authorLi, D.
dc.contributor.authorNeubert, T.
dc.contributor.authorChanrion, O.
dc.contributor.authorReglero, V.
dc.contributor.authorNavarro-González, J.
dc.contributor.authorØstgaard, Nikolai
dc.date.accessioned2023-04-04T07:52:35Z
dc.date.available2023-04-04T07:52:35Z
dc.date.created2023-01-13T13:59:28Z
dc.date.issued2022
dc.identifier.issn2169-897X
dc.identifier.urihttps://hdl.handle.net/11250/3061966
dc.description.abstractWe present nighttime worldwide distributions of key features of Blue LUminous Events (BLUEs) detected by the Modular Multispectral Imaging Array of the Atmosphere-Space Interaction Monitor. Around 10% of all detected BLUEs exhibit an impulsive single pulse shape. The rest of BLUEs are unclear (impulsive or not) single, multiple or with ambiguous pulse shapes. BLUEs exhibit two distinct populations with peak power density <25 µWm−2 (common) and ≥25 µWm−2 (rare) with different rise times and durations. The altitude (and depth below cloud tops) zonal distribution of impulsive single pulse BLUEs indicate that they are commonly present between cloud tops and a depth of ≤4 km in the tropics and ≤1 km in mid and higher latitudes. Impulsive single pulse BLUEs in the tropics are the longest (up to ∼4 km height) and have the largest number of streamers (up to ∼3 × 109). Additionally, the analysis of BLUEs has turned out to be particularly complex due to the abundance of radiation belt particles (at high latitudes and in the South Atlantic Anomaly [SAA]) and cosmic rays all over the planet. True BLUEs can not be fully distinguished from radiation belt particles and cosmic rays unless other ground-based measurements associated with the optically detected BLUEs are available. Thus, the search algorithm of BLUEs presented in Soler et al. (2021), https://doi.org/10.1029/2021gl094657 is now completed with a new additional step that, if used, can considerably smooth the SAA shadow but can also underestimate the number of BLUEs worldwide.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsNavngivelse-Ikkekommersiell 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/deed.no*
dc.titleGlobal Distribution of Key Features of Streamer 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.articlenumbere2022JD037535en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2022JD037535
dc.identifier.cristin2106636
dc.source.journalJournal of Geophysical Research (JGR): Atmospheresen_US
dc.identifier.citationJournal of Geophysical Research (JGR): Atmospheres. 2022, 127 (24), e2022JD037535.en_US
dc.source.volume127en_US
dc.source.issue24en_US


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Navngivelse-Ikkekommersiell 4.0 Internasjonal
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