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Cross-tail current - Resonant orbitsA technique to generate self-consistent 1D current sheets is described. Groups of monoenergetic protons were followed in a modified Harris magnetic field. This sample current sheet is characterized by resonant quasi-adiabatic orbits. The magnetic moment of a quasi-adiabatic ion which is injected from outside a current sheet changes substantially during the orbit but returns to almost its initial value by the time the ion leaves. Several ion and electron groups were combined to produce a plasma sheet in which the charged particles carry the currents needed to generate the magnetic field in which the orbits were traced. An electric field also is required to maintain charge neutrality. Three distinct orbit types, one involving untrapped ions and two composed of trapped ions, were identified. Limitations associated with the use of a 1D model also were investigated; it can provide a good physical picture of an important component of the cross-tail current, but cannot adequately describe any region of the magnetotail in which the principal current sheet is separated from the plasma sheet boundary layer by a nearly isotropic outer position of the central plasma sheet.
Document ID
19940033528
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Kaufmann, Richard L.
(NASA Headquarters Washington, DC United States)
Lu, Chen
(New Hampshire Univ. Durham, United States)
Date Acquired
August 16, 2013
Publication Date
September 1, 1993
Publication Information
Publication: Journal of Geophysical Research
Volume: 98
Issue: A9
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
94A10183
Funding Number(s)
CONTRACT_GRANT: NAGW-1625
CONTRACT_GRANT: NSF ATM-90-01446
CONTRACT_GRANT: NSF ATM-92-02126
Distribution Limits
Public
Copyright
Other

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