Tidally driven dynamos in a rotating sphere

TL;DR

This study demonstrates that the elliptical (tidal) instability in a rotating spherical fluid can generate large-scale magnetic fields, suggesting a potential mechanism for planetary and stellar magnetism driven by tides.

Contribution

The paper shows through global simulations that tidal-driven elliptical instability can produce large-scale magnetic fields in a spherical fluid, extending prior local studies.

Findings

Elliptical instability can drive dipole-dominated magnetic fields.

The mechanism is effective in global spherical simulations.

Tidal forces may significantly influence planetary and stellar dynamos.

Abstract

Large-scale planetary or stellar magnetic fields generated by a dynamo effect are mostly attributed to flows forced by buoyancy forces in electrically conducting fluid layers. However, these large-scale fields may also be controlled by tides, as previously suggested for the star $\tau$-boo, Mars or the Early Moon. By simulating a small local patch of a rotating fluid, \cite{Barker2014} have recently shown that tides can drive small-scale dynamos by exciting a hydrodynamic instability, the so-called elliptical (or tidal) instability. By performing global magnetohydrodynamic simulations of a rotating spherical fluid body, we investigate if this instability can also drive the observed large-scale magnetic fields. We are thus interested by the dynamo threshold and the generated magnetic field in order to test if such a mechanism is relevant for planets and stars. Rather than solving the problem in a geometry deformed by tides, we consider a spherical fluid body and add a body force to mimic the tidal deformation in the bulk of the fluid. This allows us to use an efficient spectral code to solve the magnetohydrodynamic problem. We first compare the hydrodynamic results with theoretical asymptotic results, and numerical results obtained in a truely deformed ellipsoid, which confirms the presence of the elliptical instability. We then perform magnetohydrodynamic simulations, and investigate the dynamo capability of the flow. Kinematic and self-consistent dynamos are finally simulated, showing that the elliptical instability is capable of generating dipole dominated large-scale magnetic field in global simulations of a fluid rotating sphere.