9:30 AM - 9:45 AM
[PEM17-13] Transition from microscopic to macroscopic scales in magnetic reconnection
Keywords:Magnetic reconnection, Kinetic plasma simulation, Slow shocks
A direct approach to unravel the transition from microscopic to macroscopic scales in magnetic reconnection would be very large-scale computer simulations of first-principle, fully-kinetic plasmas. However, currently-available computer resources are still not enough to fully resolve kinetic plasma at realistic macroscopic scales. As an alternative, intermediate models such as two fluid and hybrid models are utilized to cover a broader range than fully-kinetic simulations while incorporating some significant physics beyond magnetohydrodynamics (MHD). Higashimori and Hoshino (2012) conducted hybrid simulations of magnetic reconnection and argued that large temperature anisotropy in association with reconnection inhibits the formation of slow shocks anticipated in fast reconnection at the MHD scale. The temperature anisotropy will be eventually relaxed and the system is expected to approach MHD-scale reconnection.
To study the transition from microscopic to macroscopic scales in magnetic reconnection, we conduct fully-kinetic plasma simulations including artificial relaxation. Depending on simulation parameters, the velocity distribution is isotropized to mimic physical relaxation processes. By comparing simulations with and without the relaxation, we investigate its effect on the evolution of magnetic reconnection. When the relaxation is activated after the saturation of kinetic-scale reconnection, a localized diffusion region is maintained by particle inertia instead of anisotropic pressure, and a bifurcated current structure appears. This structure is identified as switch-off slow shocks, suggesting efficient energy conversion there rather than within the diffusion region. The reconnection rate remains fast even after the relaxation is activated, indicating the transition from kinetic-scale reconnection to Petscheck-type MHD-scale reconnection as a consequence of the relaxation of the velocity distribution.