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dc.contributor.authorAlm, Love
dc.contributor.authorAndré, Mats
dc.contributor.authorGraham, Daniel B.
dc.contributor.authorKhotyaintsev, Yuri V.
dc.contributor.authorVaivads, Andris
dc.contributor.authorChappell, Charles Richard
dc.contributor.authorDargent, Jérémy
dc.contributor.authorFuselier, Stephen A.
dc.contributor.authorHaaland, Stein
dc.contributor.authorLavraud, Benoit
dc.contributor.authorLi, Wenya
dc.contributor.authorTenfjord, Paul
dc.contributor.authorToledo-Redondo, Sergio
dc.contributor.authorVines, Sarah K.
dc.date.accessioned2021-03-08T11:16:21Z
dc.date.available2021-03-08T11:16:21Z
dc.date.created2020-03-15T13:09:49Z
dc.date.issued2019
dc.PublishedGeophysical Research Letters. 2019, 46 (17-18), 10230-10239.
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/2732127
dc.description.abstractWe present Magnetospheric Multiscale mission (MMS) observations of Hall physics in the magnetotail, which compared to dayside Hall physics is a relatively unexplored topic. The plasma consists of electrons, moderately cold ions (T∼1.5 keV) and hot ions (T∼20 keV). MMS can differentiate between the cold ion demagnetization region and hot ion demagnetization regions, which suggests that MMS was observing multiscale Hall physics. The observed Hall electric field is compared with a generalized Ohm's law, accounting for multiple ion populations. The cold ion population, despite its relatively high initial temperature, has a significant impact on the Hall electric field. These results show that multiscale Hall physics is relevant over a much larger temperature range than previously observed and is relevant for the whole magnetosphere as well as for other astrophysical plasma.en_US
dc.language.isoengen_US
dc.publisherWileyen_US
dc.titleMMS Observations of Multiscale Hall Physics in the Magnetotailen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2019. American Geophysical Union.en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2019GL084137
dc.identifier.cristin1801717
dc.source.journalGeophysical Research Lettersen_US
dc.source.4046
dc.source.1417-18
dc.source.pagenumber10230-10239en_US
dc.identifier.citationGeophysical Research Letters. 2019, 46 (17-18), 10230-10239.en_US
dc.source.volume46en_US
dc.source.issue17-18en_US


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