American Geophysical Union Become an AGU Member
Subscribe to AGU Journals
AGU Home AGU Publications

Read Full Article (file size: 958513 bytes)    Cited by

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109, A03205, doi:10.1029/2003JA010123, 2004

Current-driven instabilities in forced current sheets

M. I. Sitnov

Institute for Research in Electronics and Applied Physics, University of Maryland, College Park, Maryland, USA


A. T. Y. Lui

Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA


P. N. Guzdar

Institute for Research in Electronics and Applied Physics, University of Maryland, College Park, Maryland, USA


P. H. Yoon

Institute for Physical Science and Technology, University of Maryland, College Park, Maryland, USA


Abstract

The nonlocal kinetic linear stability analysis of the non-Harris thin current sheet equilibrium, namely the thin current sheet embedded in a thicker anisotropic plasma sheet [ Sitnov et al., 2000a , 2000b], with respect to current-driven instabilities is performed using the finite element technique. In contrast to the Harris sheet, the new equilibrium becomes possible due to the plasma anisotropy outside the sheet caused by two warm counterstreaming field-aligned beams and complex ion orbits that cannot be described in such thin current sheets in terms of the conventional magnetic moment. It is found that in contrast to the case of the Harris sheet, the analogs of the drift-kink instability in these current sheets can have significant growth rates for the realistic ion-to-electron mass and temperature ratios. The unstable modes share the properties with both the lower-hybrid and drift-kink modes. In particular, the unstable modes resemble the lower-hybrid drift modes as they are more highly structured across the sheet than the drift-kink instability (DKI) and assume both odd (DKI-like) and even parity solutions. On the other hand, in contrast to the lower-hybrid drift instability (LHDI) and like the DKI, the unstable modes have much larger wavelength, electromagnetic component, and significantly perturb the central current region. The possible role of the current-driven instabilities in magnetic reconnection and magnetic annihilation as well as the geophysical implications such as the current disruption in the geomagnetotail during substorms are also discussed.

Received 8 July 2003; accepted 31 December 2003; published 11 March 2004.

Index Terms: 2772 Magnetospheric Physics: Plasma waves and instabilities; 2744 Magnetospheric Physics: Magnetotail; 3230 Mathematical Geophysics: Numerical solutions; 2788 Magnetospheric Physics: Storms and substorms; 7827 Space Plasma Physics: Kinetic and MHD theory.


Read Full Article (file size: 958513 bytes)    Cited by

Citation: Sitnov, M. I., A. T. Y. Lui, P. N. Guzdar, and P. H. Yoon (2004), Current-driven instabilities in forced current sheets, J. Geophys. Res., 109, A03205, doi:10.1029/2003JA010123.