On the evolution of vortices in massive protoplanetary discs
arXiv:1805.05768 · doi:10.1093/mnras/sty1314
Abstract
It is expected that a pressure bump can be formed at the inner edge of a dead-zone, and where vortices can develop through the Rossby Wave Instability (RWI). It has been suggested that self-gravity can significantly affect the evolution of such vortices. We present the results of 2D hydrodynamical simulations of the evolution of vortices forming at a pressure bump in self-gravitating discs with Toomre parameter in the range . We consider isothermal plus non-isothermal disc models that employ either the classical prescription or a more realistic treatment for cooling. The main aim is to investigate whether the condensating effect of self-gravity can stabilize vortices in sufficiently massive discs. We confirm that in isothermal disc models with , vortex decay occurs due to the vortex self-gravitational torque. For discs with , the vortex develops gravitational instabilities within its core and undergoes gravitational collapse, whereas more massive discs give rise to the formation of global eccentric modes. In non-isothermal discs with cooling, the vortex maintains a turbulent core prior to undergoing gravitational collapse for , whereas it decays if . In models that incorpore both self-gravity and a better treatment for cooling, however, a stable vortex is formed with aspect ratio . Our results indicate that self-gravity significantly impacts the evolution of vortices forming in protoplanetary discs, although the thermodynamical structure of the vortex is equally important for determining its long-term dynamics.
Accepted in MNRAS
References in corpus (6)
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- Self-Sustaining Vortices in Protoplanetary Disks: Setting the Stage for Planetary System Formation
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