Potential vorticity dynamics in the framework of disk shallow-water theory: I. The Rossby wave instability

TL;DR

This paper investigates the Rossby wave instability in astrophysical disks using a three-dimensional disk shallow-water model, identifying conditions under which the instability occurs related to potential vorticity profiles.

Contribution

It extends the understanding of Rossby wave instability by analyzing its occurrence in a 3D disk shallow-water framework with specific potential vorticity profiles.

Findings

Instability occurs for potential vorticity depressions narrower than a maximum scale.

No instability for single or localized peak vorticity profiles.

Instability results from interaction of Rossby edgewaves.

Abstract

The Rossby wave instability in astrophysical disks is as a potentially important mechanism for driving angular momentum transport in disks. We aim to understand this instability in an approximate three-dimensional disk model environment which we assume to be a single homentropic annular layer we analyze using disk shallow-water theory. We consider the normal mode stability analysis of two kinds of radial profiles of the mean potential vorticity: The first type is a single step and the second kind is a symmetrical step of finite width describing either a localized depression or peak of the mean potential vorticity. For single potential vorticity steps we find there is no instability. There is no instability when the symmetric step is a localized peak. However, the Rossby wave instability occurs when the symmetrical step profile is a depression, which, in turn, corresponds to localized peaks in the mean enthalpy profile. This is in qualitative agreement with previous two-dimensional investigations of the instability. For all potential vorticity depressions, instability occurs for regions narrower than some maximum radial length scale. We interpret the instability as resulting from the interaction of at least two Rossby edgewaves. We identify the Rossby wave instability in the restricted three-dimensional framework of disk shallow water theory. Additional examinations of generalized barotropic flows are needed. Viewing disk vortical instabilities from the conceptual perspective of interacting edgewaves can be useful.