HR: 14:30h
AN: SM33A-05 [Abstracts]
TI: The Scaling of Forced Collisionless Reconnection
AU: * Sullivan, B P
EM: Brian.P.Sullivan@Dartmouth.edu
AF: Dartmouth College, 6127 Wilder Lab, Hanover, NH 03755 United States
AU: Rogers, B N
EM: barrett.rogers@dartmouth.edu
AF: Dartmouth College, 6127 Wilder Lab, Hanover, NH 03755 United States
AU: Shay, M A
EM: shay@glue.umd.edu
AF: Institute for Research in Electronics and Applied Physics, University of Maryland, University of
Maryland, College Park, MD 20742 United States
AB:
We present two-fluid simulations of forced magnetic
reconnection in a collisionless two-dimensional slab geometry. In the absence of forcing, our system has Δ' ≤ 0 and as expected exhibits no reconnection. The most common method of driving reconnection in such stable systems is to add a
finite amplitude perturbation to the boundaries of the simulation. In contrast, reconnection in our study is driven by a
spatially localized forcing
function, which is added to the ion momentum equation in the interior of the simulation domain. This function represents a
generic external forcing agent that drives plasma and magnetic field toward the reconnection region at a controllable rate.
We investigate the behavior of the resulting reconnection as a function of various free parameters in the system, including
the temporal and spatial
structure of the forcing function, the plasma β, and the presence of an out-of-plane guide magnetic field
component. Consistent with previous scaling studies done on systems with relatively large Δ', we find that for
sufficiently strong forcing the reconnection process becomes Alfvénic, i.e., the inflow velocity scales roughly like some
small fraction of the Alfvén speed based on the reconnecting component of the magnetic field just upstream of the
dissipation region. The magnitude of this field and thus the rate of reconnection is ultimately controlled by the behavior of the forcing function.
DE: 7835 Magnetic reconnection
SC: SPA-Magnetospheric Physics [SM]
MN: 2005 Joint Assembly