Rossby Wave Instability with Self-Gravity
R. V. E. Lovelace, R. G. Hohlfeld

TL;DR
This paper investigates how self-gravity influences the Rossby wave instability in thin discs, identifying key parameters that determine stability and providing criteria for when self-gravity must be considered in models.
Contribution
It extends the analysis of Rossby wave instability to include self-gravity effects across a range of disc models, deriving conditions for instability based on disc parameters.
Findings
Self-gravity significantly affects instability for low Toomre Q values and certain azimuthal wavenumbers.
Instability can occur at surface density depressions or bumps depending on self-gravity and Q.
Self-gravity is negligible for high Q discs with certain mode numbers, simplifying modeling efforts.
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…
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