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dc.contributor.authorElhawary, Reham Zakaria Ahmed Mohamed
dc.contributor.authorLaundal, Karl Magnus
dc.contributor.authorReistad, Jone Peter
dc.contributor.authorHatch, Spencer Mark
dc.date.accessioned2023-03-08T13:16:25Z
dc.date.available2023-03-08T13:16:25Z
dc.date.created2022-05-31T15:07:40Z
dc.date.issued2022
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3057101
dc.description.abstractAuroral substorm onset locations are highly unpredictable. Previous studies have shown that the By component of the interplanetary magnetic field (IMF) explains ∼5% of the variation in onset magnetic local time (MLT), while solar wind conditions and the other IMF components have even less explanatory power. In this study, we show that the level of geomagnetic activity before substorm onset, as indicated by the AL index, explains an additional ∼5% of the variation in onset MLT. We discuss our results with regard to recent modeling studies, which show that gradients in the ionospheric Hall conductance can lead to a duskward shift of the magnetotail dynamics. Our findings suggest that this magnetosphere-ionosphere coupling effect may also influence the location of substorm onsets.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.titlePossible Ionospheric Influence on Substorm Onset Locationen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2022 The Author(s)en_US
dc.source.articlenumbere2021GL096691en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2021GL096691
dc.identifier.cristin2028499
dc.source.journalGeophysical Research Lettersen_US
dc.relation.projectNorges forskningsråd: 300844en_US
dc.identifier.citationGeophysical Research Letters. 2022, 49 (4), e2021GL096691.en_US
dc.source.volume49en_US
dc.source.issue4en_US


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Navngivelse-Ikkekommersiell 4.0 Internasjonal
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