Earthward flowing plasmoid: Structure and its related ionospheric signature

dc.contributor.authorZong, Q.-G.
dc.contributor.authorFu, S. Y.
dc.contributor.authorBaker, D. N.
dc.contributor.authorGoldstein, Melvyn
dc.contributor.authorSong, P.
dc.contributor.authorSlavin, J. A.
dc.contributor.authorFritz, T. A.
dc.contributor.authorCao, J. B.
dc.contributor.authorAmm, O.
dc.contributor.authorFrey, H.
dc.contributor.authorKorth, A.
dc.contributor.authorDaly, P. W.
dc.contributor.authorReme, H.
dc.contributor.authorPedersen, A.
dc.date.accessioned2023-11-13T19:55:00Z
dc.date.available2023-11-13T19:55:00Z
dc.date.issued2007-07-07
dc.description.abstractAn earthward moving plasmoid has been observed on 28 October 2002 by the Cluster spacecraft with simultaneous auroral viewing by the IMAGE satellite. This offers the opportunity to ascertain the optical and the evolutional signatures in the ionosphere of the earthward moving plasmoid. The ionospheric signatures observed in this paper are not substorm-related. Both the ground-based measurements and IMAGE satellite auroral observations show the ionospheric signatures moving to lower latitudes, when the earthward moving plasmoid is observed by the Cluster spacecraft. The intensity of the current in the center of the plasmoid is found to be weaker than that in the adjacent region. Also, the directions of the current in the central part of the plasmoid, different from the background cross-tail current, are more field-aligned. Those facts are consistent with the tail current closes through the substorm-like current wedge, since the cross-tail current is blocked by the plasmoid. On the other hand, the current in the earthward plasmoid may close through the interhemisphere. In this paper we demonstrate that the magnetic structures, plasmoids and flux ropes, will transport flux and energy from the distant tail to the Earth.en_US
dc.description.sponsorshipThis work is partly supported by NSFC projects 40528005 and 40374060 and by the CAS International Partnership Program for Creative Research Team.en_US
dc.description.urihttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2006JA012112en_US
dc.format.extent8 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m2bltz-qlqb
dc.identifier.citationZong, Q.-G., et al. (2007), Earthward flowing plasmoid: Structure and its related ionospheric signature, J. Geophys. Res., 112, A07203, doi:10.1029/2006JA012112.en_US
dc.identifier.urihttps://doi.org/10.1029/2006JA012112
dc.identifier.urihttp://hdl.handle.net/11603/30748
dc.language.isoen_USen_US
dc.publisherAGUen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Goddard Planetary Heliophysics Institute (GPHI)
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.en_US
dc.rightsPublic Domain Mark 1.0*
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleEarthward flowing plasmoid: Structure and its related ionospheric signatureen_US
dc.typeTexten_US
dcterms.creatorhttps://orcid.org/0000-0002-5317-988Xen_US

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