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Detailed Reference Information |
Burkhart, G.R., Drake, J.F., Dusenbery, P.B. and Speiser, T.W. (1992). Ion tearing in a magnetotail configuration with an embedded thin current sheet. Journal of Geophysical Research 97: doi: 10.1029/92JA01523. issn: 0148-0227. |
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The 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 (&lgr;0/Lz)2, where Lz is the overall half thickness of the plasma sheet, &lgr;0 is the ion inertial length, c/&ohgr;pi, and &ohgr;pi is the ion plasma frequency at the neutral sheet edge. In the absence of the current outside the neutral sheet, current filamentation is stable. ¿ American Geophysical Union 1992 |
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Abstract |
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Keywords
Magnetospheric Physics, Storms and substorms, Magnetospheric Physics, Magnetotail, Interplanetary Physics, Discontinuities |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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