On the Time Variability of Geometrically-Thin Black Hole Accretion Disks II: Viscosity-Induced Global Oscillation Modes in Simulated Disks

TL;DR

This study investigates viscosity-driven oscillations in simulated thin black hole accretion disks, revealing trapped global modes that could explain observed high-frequency quasi-periodic oscillations, contrasting with MHD simulation results.

Contribution

It demonstrates the existence of viscosity-induced trapped global oscillation modes in simulated thin disks, highlighting differences from magnetohydrodynamic simulations and suggesting new avenues for observational detection.

Findings

Viscous disks develop trapped global oscillation modes similar to g-modes and p-modes.

Oscillations propagate outward from the inner disk regions.

Magnetohydrodynamic simulations do not show these trapped modes.

Abstract

We examine the evolution and influence of viscosity-induced diskoseismic modes in simulated black hole accretion disks. Understanding the origin and behavior of such oscillations will help us to evaluate their potential role in producing astronomically observed high-frequency quasi-periodic oscillations in accreting black hole binary systems. Our simulated disks are geometrically-thin with a constant half-thickness of five percent the radius of the innermost stable circular orbit. A pseudo-Newtonian potential reproduces the relevant effects of general relativity, and an alpha-model viscosity achieves angular momentum transport and the coupling of orthogonal velocity components in an otherwise ideal hydrodynamic numerical treatment. We find that our simulated viscous disks characteristically develop and maintain trapped global mode oscillations with properties similar to those expected of trapped g-modes and inner p-modes in a narrow range of frequencies just below the maximum radial epicyclic frequency. Although the modes are driven in the inner portion of the disk, they generate waves that propagate at the trapped mode frequencies out to larger disk radii. This finding is contrasted with the results of global magnetohydrodynamic disk simulations, in which such oscillations are not easily identified. Such examples underscore fundamental physical differences between accretion systems driven by the magneto-rotational instability and those for which alpha viscosity serves as a proxy for the physical processes that drive accretion, and we explore potential approaches to the search for diskoseismic modes in full magnetohydrodynamic disks.