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dc.contributor.authorLessard, Marc R.
dc.contributor.authorFritz, Bruce
dc.contributor.authorSadler, Brent
dc.contributor.authorCohen, Ian J.
dc.contributor.authorKenward, David
dc.contributor.authorGodbole, Niharika
dc.contributor.authorClemmons, James H.
dc.contributor.authorHecht, James H.
dc.contributor.authorLynch, Kristina A.
dc.contributor.authorHarrington, Meghan
dc.contributor.authorRoberts, Thomas M.
dc.contributor.authorHysell, David
dc.contributor.authorCrowley, Geoff
dc.contributor.authorSigernes, Fred
dc.contributor.authorSyrjäsuo, Mikko
dc.contributor.authorEllingsen, Pål Gunnar
dc.contributor.authorPartamies, Noora
dc.contributor.authorMoen, Jøran Idar
dc.contributor.authorClausen, Lasse Boy Novock
dc.contributor.authorOksavik, Kjellmar
dc.contributor.authorYeoman, Timothy
dc.date.accessioned2021-05-28T10:58:16Z
dc.date.available2021-05-28T10:58:16Z
dc.date.created2020-11-19T20:24:03Z
dc.date.issued2020
dc.PublishedGeophysical Research Letters. 2020, 47 (21), 1-7.
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/2756862
dc.description.abstractThe Rocket Experiment for Neutral Upwelling 2 (RENU2) rocket was launched on 13 December 2015 at 07:34 UT. The payload transited the cusp region during a neutral upwelling event, supported by a comprehensive set of onboard and ground-based instrumentation. RENU2 data highlight two important processes. One is that a proper understanding of neutral upwelling by Poleward Moving Auroral Forms (PMAFs) requires a treatment that mimics the quasiperiodic passage of a sequence of PMAFs. As a PMAF reaches a flux tube, its physical consequences must be determined including the residual history of effects from previous passages, implying that understanding such a process requires an accounting of the system hysteresis. Second, RENU2 observations suggest that neutral density enhancements driven by precipitation and/or Joule heating can be highly structured in altitude and latitude. In addition, timescales involving neutral dynamics suggest that the structuring must be slowly changing, for example, over the course of 10 to tens of minutes.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.titleOverview of the Rocket Experiment for NeutralUpwelling Sounding Rocket 2 (RENU2)en_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2019 American Geophysical Union. All Rights Reserved.en_US
dc.source.articlenumbere2018GL081885en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2018GL081885
dc.identifier.cristin1850097
dc.source.journalGeophysical Research Lettersen_US
dc.source.4047
dc.source.1421
dc.identifier.citationGeophysical Research Letters. 2020, 47(21), e2018GL081885en_US
dc.source.volume47en_US
dc.source.issue21en_US


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