Evidence of active MHD instability in EULAG-MHD simulations of solar convection

TL;DR

This study identifies active magnetohydrodynamical instabilities in EULAG-MHD solar convection simulations, suggesting these instabilities influence magnetic cycle dynamics and magnetic field dissipation.

Contribution

It provides evidence for non-axisymmetric magnetoshear and Tayler instabilities in solar-like MHD simulations, highlighting their role in magnetic cycle modulation.

Findings

Detection of non-axisymmetric magnetoshear instability.

Evidence for Tayler instability at high latitudes.

Magnetic cycle period may be affected by MHD instabilities.

Abstract

We investigate the possible development of magnetohydrodynamical instabilities in the EULAG-MHD "millenium simulation" of Passos & Charbonneau (2014). This simulation sustains a large-scale magnetic cycle characterized by solar-like polarity reversals taking place on a regular multidecadal cadence, and in which zonally-oriented bands of strong magnetic field accumulate below the convective layers, in response to turbulent pumping from above in successive magnetic half-cycles. Key aspects of this simulation include low numerical dissipation and a strongly subadiabatic fluid layer underlying the convectively unstable layers corresponding to the modeled solar convection zone. These properties are conducive to the growth and development of two-dimensional instabilities otherwise suppressed by stronger dissipation. We find evidence for the action of a non-axisymmetric magnetoshear instability operating in the upper portions of the stably stratified fluid layers. We also investigate the possibility that the Tayler instability may be contributing to the destabilization of the large-scale axisymmetric magnetic component at high latitudes. On the basis of our analyses, we propose a global dynamo scenario whereby the magnetic cycle is driven primarily by turbulent dynamo action in the convecting layers, but MHD instabilities accelerate the dissipation of the magnetic field pumped down into the overshoot and stable layers, thus perhaps significantly influencing the magnetic cycle period. Support for this scenario is found in the distinct global dynamo behaviors observed in an otherwise identical EULAG-MHD simulations, using a different degree of subadiabaticity in the stable fluid layers underlying the convection zone.