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dc.contributor.authorMoser, Chrystal
dc.contributor.authorLaBelle, James William
dc.contributor.authorHatch, Spencer Mark
dc.contributor.authorMoen, Jøran Idar
dc.contributor.authorSpicher, Andres
dc.contributor.authorTakahashi, Toru
dc.contributor.authorKletzing, Craig A.
dc.contributor.authorBounds, Scott Randolph
dc.contributor.authorOksavik, Kjellmar
dc.contributor.authorSigernes, Fred
dc.contributor.authorYeoman, Timothy K.
dc.date.accessioned2021-06-02T10:32:24Z
dc.date.available2021-06-02T10:32:24Z
dc.date.created2020-12-10T07:52:52Z
dc.date.issued2021
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/2757356
dc.description.abstractAuroral whistler‐mode radio emissions called saucers are of fundamental interest because they require an unusually stationary emission process in the dynamic auroral environment, and it is a mystery how that can happen in this or similar conditions elsewhere in geospace. The Cusp Alfvén and Plasma Electrodynamics Rocket (CAPER‐2), launched into the cusp, obtained the first rocket measurements of a large‐scale, multiple‐armed dayside saucer, similar to those observed by the DEMETER satellite, with the addition of particle measurements and ground‐based measurements. Analysis of saucer shapes, directional measurements using waveforms, and ground‐based data show that, accounting for estimated uncertainties, these originate at altitudes ∼4,000 km within the cusp, the eastern side of which is penetrated by the rocket ∼100 s after the saucers are encountered. On‐board particle instruments show dispersed electron bursts in the cusp, Alfvénically accelerated at altitudes at or above the saucer sources.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.relation.urihttps://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2020GL090747
dc.titleThe Cusp as a VLF Saucer Source: First Rocket Observations of Long‐Duration VLF Saucers on the Daysideen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2020. American Geophysical Union. All Rights Reserved.en_US
dc.source.articlenumbere2020GL090747en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2020GL090747
dc.identifier.cristin1858134
dc.source.journalGeophysical Research Lettersen_US
dc.relation.projectNorges forskningsråd: 223252en_US
dc.identifier.citationGeophysical Research Letters. 2021, 48(2), e2020GL090747en_US
dc.source.volume48en_US
dc.source.issue2en_US


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