Formation, Survival, and Destruction of Vortices in Accretion Disks

TL;DR

This paper investigates the formation and stability of vortices in 3D accretion disks, revealing that only weak vortices with large azimuthal extent survive, impacting dust trapping and angular momentum transport.

Contribution

It derives the conditions for vortex survival in 3D disks, showing that vortex azimuthal extent relative to scale height determines stability, and explains previous simulation results.

Findings

Weak vortices can trap dust and aid planet formation.

Strong vortices are unstable and decay in 3D disks.

Vortex survival depends on azimuthal extent exceeding the disk's scale height.

Abstract

Two dimensional hydrodynamical disks are nonlinearly unstable to the formation of vortices. Once formed, these vortices essentially survive forever. What happens in three dimensions? We show with pseudospectral simulations that in 3D a vortex in a short box forms and survives just as in 2D. But a vortex in a tall box is unstable and is destroyed. In our simulation, the unstable vortex decays into a transient turbulent-like state that transports angular momentum outward at a nearly constant rate for hundreds of orbital times. The 3D instability that destroys vortices is a generalization of the 2D instability that forms them. We derive the conditions for these nonlinear instabilities to act by calculating the coupling between linear modes, and thereby derive the criterion for a vortex to survive in 3D as it does in 2D: the azimuthal extent of the vortex must be larger than the scale height of the accretion disk. When this criterion is violated, the vortex is unstable and decays. Because vortices are longer in azimuthal than in radial extent by a factor that is inversely proportional to their excess vorticity, a vortex with given radial extent will only survive in a 3D disk if it is sufficiently weak. This counterintuitive result explains why previous 3D simulations always yielded decaying vortices: their vortices were too strong. We conclude that in protoplanetary disks weak vortices can trap dust and serve as the nurseries of planet formation. Decaying strong vortices might be responsible for the outwards transport of angular momentum that is required to make accretion disks accrete.