Evidence of high-latitude reconnecting during northward IMF: Hawkeye observations

dc.contributor.authorKessel, R. L.
dc.contributor.authorChen, S.-H.
dc.contributor.authorGreen, J. L.
dc.contributor.authorFung, S. F.
dc.contributor.authorBoardsen, S. A.
dc.contributor.authorTan, Lun C.
dc.contributor.authorEastman, T. E.
dc.contributor.authorCraven, J. D.
dc.contributor.authorFrank, L. A.
dc.date.accessioned2021-07-30T18:09:06Z
dc.date.available2021-07-30T18:09:06Z
dc.date.issued1996-03-01
dc.description.abstractReconnection is accepted as an important process for driving the solar wind/magnetospheric interaction although it is not fully understood. In particular, reconnection for northward interplanetary magnetic field (IMF) at high-latitudes tailward of the cusp, has received little attention in comparison with equatorial reconnection for southward IMF. Using Hawkeye data we present the first direct observations of reconnection at the high-latitude magnetopause (75°) during northward IMF in the form of sunward flowing protons. This flow is nearly field aligned, approximately Alfvénic, and roughly obeys tangential momentum balance. The magnetic field shear is large at the magnetopause and there is a non-zero BN component suggesting the existence of a rotational discontinuity and reconnection. The Hawkeye observations support several recent simulations at least qualitatively in terms of flow directions expected for high-latitude reconnection during northward IMF.en
dc.description.sponsorshipWe thank the NSSDC for supply- ing the Hawkeye, IMP-8, and OMNI data. We thank J. Van Allen for making the Hawkeye data available to NSSDC. S.-H. C. acknowledges support front NAS/NRC Research Program. We thank D. Sibeck for useful commentsen
dc.description.urihttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/95GL03083en
dc.format.extent4 pagesen
dc.genrejournal articlesen
dc.identifierdoi:10.13016/m2tus4-rama
dc.identifier.citationKessel, R. L. et al.; Evidence of high-latitude reconnecting during northward IMF: Hawkeye observations; Geophysical Research Letters, 23, 5, p 583-586, 1 March, 1996; https://doi.org/10.1029/95GL03083en
dc.identifier.urihttps://doi.org/10.1029/95GL03083
dc.identifier.urihttp://hdl.handle.net/11603/22231
dc.language.isoenen
dc.publisherAmerican Geophysical Unionen
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
dc.rightsPublic Domain Mark 1.0*
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleEvidence of high-latitude reconnecting during northward IMF: Hawkeye observationsen
dc.typeTexten

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