Linear dynamics of weakly viscous accretion disks: A disk analog of Tollmien-Schlichting waves

TL;DR

This paper explores viscous instabilities in accretion disks, revealing a disk analog of Tollmien-Schlichting waves through boundary condition analysis and weak viscosity effects, offering new insights into disk dynamics.

Contribution

It introduces a novel perspective on disk instabilities by identifying a Tollmien-Schlichting wave analog in viscous accretion disks under specific boundary conditions.

Findings

Identified a disk analog of Tollmien-Schlichting waves.

Demonstrated instability persists with realistic boundary conditions.

Found that a Froude number greater than one is necessary for instability onset.

Abstract

This paper discusses new perspectives and approaches to the problem of disk dynamics where, in this study, we focus on the effects of viscous instabilities influenced by boundary effects. The Boussinesq approximation of the viscous large shearing box equations is analyzed in which the azimuthal length scale of the disturbance is much larger than the radial and vertical scales. We examine the stability of a non-axisymmetric potential vorticity mode, i.e. a PV-anomaly. in a configuration in which buoyant convection and the strato-rotational instability do not to operate. We consider a series of boundary conditions which show the PV-anomaly to be unstable both on a finite and semi-infinite radial domains. We find these conditions leading to an instability which is the disk analog of Tollmien-Schlichting waves. When the viscosity is weak, evidence of the instability is most pronounced by the emergence of a vortex sheet at the critical layer located away from the boundary where the instability is generated. For some boundary conditions a necessary criterion for the onset of instability for vertical wavelengths that are a sizable fraction of the layer's thickness and when the viscosity is small is that the appropriate Froude number of the flow be greater than one. This instability persists if more realistic boundary conditions are applied, although the criterion on the Froude number is more complicated. The unstable waves studied here share qualitative features to the instability seen in rotating Blasius boundary layers. The implications of these results are discussed. An overall new strategy for exploring and interpreting disk instability mechanisms is also suggested.