Three-dimensional Simulations of the Parker Instability in a Uniformly-rotating Disk

Astronomy and Astrophysics – Astrophysics

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Accepted for publication in ApJ, 26 text pages with 9 figures

Scientific paper

10.1086/321634

We investigate the effects of rotation on the evolution of the Parker instability in an exponentially-stratified and uniformly-rotating magnetized gas disk by carrying out three-dimensional numerical simulations with an isothermal magnetohydrodynamic code. The instability has been initialized by random velocity perturbations. In the linear stage, the evolution is not much different from that without rotation and the mixed (undular + interchange) mode regulates the system. The interchange mode induces alternating dense and rarefied regions with small radial wavelengths, while the undular mode bends the magnetic field lines in the plane of azimuthal and vertical directions. In the nonlinear stage, flow motion overall becomes chaotic as in the case without rotation. However, as the gas in higher positions slides down along field lines forming supersonic flows, the Coriolis force becomes important. As oppositely directed flows fall into valleys along both sides of magnetic field lines, they experience the Coriolis force toward opposite directions, which twists magnetic field lines there. Hence, we suggest that the Coriolis force plays a role in randomizing magnetic field. The three-dimensional density structure formed by the instability is still sheet-like with the short dimension along the radial direction, as in the case without rotation. However, the long dimension is now slightly tilted with respect to the mean field direction. The shape of high density regions is a bit rounder. The maximum enhancement factor of the vertical column density relative to its initial value is about 1.5, which is smaller than that in the case without rotation. We conclude that uniform rotation doesn't change our point of view that the Parker instability alone is not a viable mechanism for the formation of giant molecular clouds.

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