HR: 0800h
AN: SM31D-0659 [Abstracts]
TI: Electron-magnetohydrodynamic Simulations of Collisionless Reconnection in Thin Current Sheets
AU: * Jain, N
EM: njain@astro.umd.edu
AF: University of Maryland, Department of Astronomy, College Park, MD 20742, United States
AU: Sharma, A S
EM: ssh@astro.umd.edu
AF: University of Maryland, Department of Astronomy, College Park, MD 20742, United States
AB:
Recent simulations of collisionless reconnection and spacecraft observations in the
magnetotail and magnetopause have shown the existence of very thin
electron current sheets, with scale lengths of the order of a few
electron skin depths. The stability of such current sheets is crucial to the understanding
of the onset of reconnection. A two-dimensional electron-magnetohydrodynamic (EMHD) model is used to
simulate the dynamics on such short space and time scales.
The simulations of a thin electron current sheet with anti-parallel
magnetic field show the development of whistler-like perturbations,
leading to magnetic reconnection. In the EMHD model,
reconnection of field lines is facilitated by electron inertia which
provides the non-ideal effect in Ohm's law and breaks the frozen-in
condition. The whistler mode structure and growth rate are
obtained from the numerical solutions of the eigen-mode equations
derived from the linearized EMHD model. These agree well with the full
simulations, confirming the instability of the whistler-like mode.
The linear eigen-mode analysis shows that
modes with wavelengths smaller than the equilibrium scale length are stable, while those of
the order of or greater than the equilibrium scale length are unstable. The growth
rate reduces monotonically with the ratio of equilibrium scale length and electron skin depth,
indicating that the instability is driven by finite electron inertia.
The simulation shows that the instability
initiates the reconnection of the field lines, with the reconnection rate
determined by the growth rate of the instability. As the reconnection progresses the
out of plane magnetic field develops a quadrupole structure over the reconnection region.
The reconnection slows down with the saturation of
the instability, and the initial single peak of the electron current sheet
develops multiple peaks and its magnitude is reduced, yielding a bifurcated
current sheet. Three-dimensional studies are in progress and will be compared with these results.
DE: 2723 Magnetic reconnection (7526, 7835)
DE: 2744 Magnetotail
DE: 2764 Plasma sheet
SC: SPA-Magnetospheric Physics [SM]
MN: 2007 Fall Meeting