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Observations of plasmas associated with the magnetic signature of a plasmoid in the distant magnetotail
Author(s) -
Frank L. A.,
Paterson W. R.,
Ackerson K. L.,
Kokubun S.,
Yamamoto T.,
Fairfield D. H.,
Lepping R. P.
Publication year - 1994
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/94gl01604
Subject(s) - plasmoid , physics , magnetic field , electron , earth's magnetic field , magnetic reconnection , plasma , geophysics , atomic physics , computational physics , nuclear physics , quantum mechanics
The three‐dimensional electron and positive ion velocity distributions were examined for four events for which the magnetic signature of plasmoids occurred at the Geotail spacecraft position in Earth's distant magnetotail. The proton bulk parameters and the electron velocity distributions for one of the events are presented in order to characterize the qualitative character of the set of events. The north‐to‐south turnings of the magnetic field that were taken for evidence of the passage of a plasmoid were often accompanied by a significant strong core of B y that was centered on the transition of B z from north to south. The magnetic signatures thus appeared to be more indicative of flux ropes than of classical plasmoids with weak core fields. The proton and electron bulk velocities in these magnetic structures are not equal, a situation that provides an earthward current. The plasma β was typically one or greater. Counterstreaming of low‐energy electrons was often found on the magnetic field lines around the central magnetic core and suggested the existence of a closed field line topology in these regions. These events appeared to be the tailward flowing debris from acceleration processes occurring in the vicinity of a separator positioned nearer to Earth.