Dynamo Confinement of a Radiatively Spreading Solar Tachocline Revealed by Self-consistent Global Simulations
Loren I. Matilsky, Lydia Korre, Nicholas H. Brummell

TL;DR
This study demonstrates through self-consistent global simulations that a dynamo-generated magnetic field can confine the solar tachocline against radiative spreading, explaining its observed thinness.
Contribution
First to show a self-consistent simulation of a magnetically confined tachocline in a solar-like radiative spreading regime.
Findings
Magnetic confinement persists over multiple cycles.
A novel skin effect allows magnetic fields to penetrate the radiative zone.
Dynamo-generated Maxwell stress maintains tachocline thinness.
Abstract
The helioseismically observed solar tachocline is a thin internal boundary layer of shear that separates the rigidly-rotating solar radiative zone from the differentially-rotating convective zone and is believed to play a central role in the 22-year solar dynamo cycle. The observed thinness of the tachocline has long been a mystery, given the expected tendency of such shear to undergo radiative spreading. Radiative spreading is the process by which the meridional circulation and angular velocity burrow into a stably-stratified fluid owing to the mitigating effect of radiative thermal diffusion. A confinement mechanism is thus required to keep the tachocline so thin. In previous work using global dynamo simulations, we achieved a statistically-stationary confined tachocline where the confinement mechanism was derived from the Maxwell stress arising from a dynamo-generated nonaxisymmetric…
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