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dc.contributor.authorHåland, Stein Egil
dc.contributor.authorHasegawa, Hiroshi
dc.contributor.authorPaschmann, G
dc.contributor.authorSonnerup, B. U. Ö.
dc.contributor.authorDunlop, M. W.
dc.date.accessioned2022-01-25T12:07:52Z
dc.date.available2022-01-25T12:07:52Z
dc.date.created2021-09-03T09:26:50Z
dc.date.issued2021
dc.identifier.issn2169-9380
dc.identifier.urihttps://hdl.handle.net/11250/2839207
dc.description.abstractThe terrestrial magnetopause forms the boundary between the solar wind plasma with its embedded interplanetary magnetic field on one side, and the terrestrial magnetosphere, dominated by Earth's dipole field, on the other side. It is therefore a key region for the transfer of mass, momentum, and energy from the solar wind to the magnetosphere. The Cluster mission, comprising a constellation of four spacecraft flying in formation was launched more than 20 years ago to study boundaries in space. During its lifetime, Cluster has provided a wealth of new knowledge about the magnetopause. In this paper, we give an overview of Cluster-based studies of this boundary, and highlight a selection of interesting results.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.title20 Years of Cluster Observations: The Magnetopause,en_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2021 The Author(s)en_US
dc.source.articlenumbere2021JA029362en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2021JA029362
dc.identifier.cristin1931037
dc.source.journalJournal of Geophysical Research (JGR): Space Physicsen_US
dc.relation.projectNorges forskningsråd: 223252en_US
dc.identifier.citationJournal of Geophysical Research (JGR): Space Physics. 2021, 126, e2021JA029362en_US
dc.source.volume126en_US
dc.source.issue8en_US


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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