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Ion tearing in a magnetotail configuration with an embedded thin current sheetThe ion tearing instability is investigated in a magnetotail configuration that consists of a diffuse plasma sheet current and an embedded, thin current sheet with a strong current. For historical reasons, the thin embedded current sheet will be called a 'neutral sheet', even though the normal component of the magnetic field, Bn, is nonzero. In particular, we assume that the current within the thin current sheet is due to the acceleration of 'Speiserlike' ion trajectories by a cross-tail electric field Ey. It is found that the strong current within the neutral sheet is essentially unimportant to the growth rate of the tearing instability, and that the growth rate scales as (lambda(0)/Lz) squared, where Lz is the overall half thickness of the plasma sheet and lambda (0) is the ion inertial length. In the absence of the current outside the neutral sheet, current filamentation is stable.
Document ID
19930032329
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Burkhart, G. R.
(Colorado Univ.; NOAA, Space Environment Lab., Boulder, United States)
Drake, J. F.
(Maryland Univ. College Park, United States)
Dusenbery, P. B.
(NASA Headquarters Washington, DC United States)
Speiser, T. W.
(Colorado Univ.; NOAA, Space Environment Lab., Boulder, United States)
Date Acquired
August 15, 2013
Publication Date
November 1, 1992
Publication Information
Publication: Journal of Geophysical Research
Volume: 97
Issue: A11
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
93A16326
Funding Number(s)
CONTRACT_GRANT: NSF ATM-91-12954
CONTRACT_GRANT: NAGW-1176
CONTRACT_GRANT: NAGW-2079
CONTRACT_GRANT: NAG5-1506
Distribution Limits
Public
Copyright
Other

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