paper

Rossby Wave Instability with Self-Gravity

arXiv:1212.0443 · doi:10.1093/mnras/sts361

Abstract

The Rossby wave instability (RWI) in non-self-gravitating discs can be triggered by a bump at a radius in the disc surface mass-density (which is proportional to the inverse potential vorticity). It gives rise to a growing non-axisymmetric perturbation [, ] in the vicinity of consisting of anticyclonic vortices which may facilitate planetesimal growth in protoplanetary discs. Here, we analyze a continuum of thin disc models ranging from self-gravitating to non-selfgravitating. The key quantities determining the stability/instability are: (1) the parameters of the bump (or depression) in the disc surface density, (2) the Toomre parameter of the disc (a non-self-gravitating disc has ), and (3) the dimensionless azimuthal wavenumber of the perturbation , where is the half-thickness of the disc. For discs stable to axisymmetric perturbations (), the self-gravity has a significant role for or ; instability may occur for a depression or groove in the surface density if . For the self-gravity is not important, and instability may occur at a bump in the surface density. Thus, for all mode numbers , the self-gravity is unimportant for . We suggest that the self-gravity be included in simulations for cases where .

5 pages, 5 figures

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