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Pritchett et al. 1996
Pritchett, P.L., Coroniti, F.V. and Decyk, V.K. (1996). Three-dimensional stability of thin quasi-neutral current sheets. Journal of Geophysical Research 101: doi: 10.1029/96JA02665. issn: 0148-0227.

In a thin current sheet (&rgr;i0/L≲1, where &rgr;i0 is the ion gyroradius in the lobe field and L is the current sheet half thickness) of the generalized Harris type, the relative ion-electron cross-field drift is comparable to the ion thermal velocity. The three-dimensional stability properties of such a thin current sheet are investigated by means of nonlocal two-fluid theory and two-dimensional and three-dimensional full particle simulations. As was suggested originally by Zhu et al. [1992>, the drift kink mode is found to be of critical importance. For the simple case of no initial Bz field the fluid theory demonstrates that the drift kink mode is a non-MHD mode with a polarization structure such that E1y is an antisymmetric function of z while E1z is a symmetric function with E1z(0)≠0. Two-dimensional (y,z) particle simulations indicate that the nonlinear behavior of this mode is dominated by long-wavelength modes with kyL~1 and frequency &ohgr;&tgr;~&OHgr;i0, where &OHgr;i0 is the ion gyrofrequency in the lobe field. Three-dimensional particle simulations performed on a massively parallel computer show that while the growth rates for the drift kink mode are reduced by the finite Bz, they can still be appreciable (&ggr;/&OHgr;i0≲0.05--0.10). The kyL~1 drift kink modes are always the first to grow in the simulations; subsequently, tearing-like modes with a dominant kx wave vector also become unstable. Implications of these results for the triggering of substorms are discussed. ¿ American Geophysical Union 1996

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Abstract

Keywords
Magnetospheric Physics, Magnetotail, Magnetospheric Physics, Plasma waves and instabilities, Magnetospheric Physics, Plasma sheet, Space Plasma Physics, Magnetic reconnection
Journal
Journal of Geophysical Research
http://www.agu.org/journals/jb/
Publisher
American Geophysical Union
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