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dc.contributor.authorKolstø, Håkon Midthun
dc.contributor.authorNorgren, Astrid Elisabet Cecilia
dc.contributor.authorHesse, Michael
dc.contributor.authorChen, Li-Jen
dc.contributor.authorTenfjord, Paul
dc.contributor.authorSpinnangr, Susanne Flø
dc.contributor.authorKwagala, Norah Kaggwa
dc.date.accessioned2021-10-27T08:43:42Z
dc.date.available2021-10-27T08:43:42Z
dc.date.created2021-09-20T17:35:43Z
dc.date.issued2021
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/2825896
dc.description.abstractHeavier plasma species such as oxygen ions can have a large impact on the magnetic reconnection process. It has been hypothesized that the acceleration of demagnetized oxygen ions by the Hall electric field will lead to the formation of an oxygen wave that expands into the exhaust. By comparing data from NASA's Magnetospheric Multiscale mission to a fully kinetic particle-in-cell simulation, we can for the first time provide observational evidence of such an expanding oxygen wave. The wave is characterized by an oxygen jet consisting of cold ions directed toward the neutral sheet associated with a density cavity. This density cavity forms as the O+ are subject to collective acceleration by the Hall electric field leaving behind a region of low-density oxygen ions. Our results are important for the understanding of the role and effect of oxygen ions in magnetic reconnection.en_US
dc.language.isoengen_US
dc.publisherAmerican Geophysical Unionen_US
dc.rightsNavngivelse-Ikkekommersiell 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/deed.no*
dc.titleMagnetospheric Multiscale Observations of an Expanding Oxygen Wave in Magnetic Reconnectionen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2021 the authorsen_US
dc.source.articlenumbere2021GL095065en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doihttps://doi.org/10.1029/2021GL095065
dc.identifier.cristin1936274
dc.source.journalGeophysical Research Lettersen_US
dc.identifier.citationGeophysical Research Letters. 2021, 48 (19), e2021GL095065.en_US
dc.source.volume48en_US
dc.source.issue19en_US


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Navngivelse-Ikkekommersiell 4.0 Internasjonal
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