Abstract

Our global 3D simulations of convection and dynamo action in a Sun-like star reveal that persistent wreaths of strong magnetism can be built within the bulk of the convention zone. Here we examine the characteristics of buoyant magnetic structures that are self-consistently created by dynamo action and turbulent convective motions in a simulation with solar stratification but rotating at three times the current solar rate. These buoyant loops originate within sections of the magnetic wreaths in which turbulent flows amplify the fields to much higher values than is possible through laminar processes. These amplified portions can rise through the convective layer by a combination of magnetic buoyancy and advection by convective giant cells, forming buoyant loops. We measure statistical trends in the polarity, twist, and tilt of these loops. Loops are shown to preferentially arise in longitudinal patches somewhat reminiscent of active longitudes in the Sun, although broader in extent. We show that the strength of the axisymmetric toroidal field is not a good predictor of the production rate for buoyant loops or the amount of magnetic flux in the loops that are produced.

Highlights

  • We show that the strength of the axisymmetric toroidal field is not a good predictor of the production rate for buoyant loops or the amount of magnetic flux in the loops that are produced

  • In many mean-field models it is assumed that buoyant magnetic flux at a given latitude and time is proportional to the axisymmetric toroidal field strength at that location and time at the generation depth

  • This article has explored the first global convective-dynamo simulation to achieve buoyant magnetic loops that transport coherent magnetic structures through the convection zone. These buoyant structures arise from large-scale magnetic wreaths, which have been previously described in both persistent (Brown et al, 2010) and cyclic states (Brown et al, 2011; Nelson et al, 2013)

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Summary

Flux Emergence and Convective Dynamos

Convective dynamo action in the interior of the Sun is the source of the magnetism that creates sunspots and drives space weather. Turning to dynamo action achieved in an MHD simulation in such stars at 3 , Brown et al (2010) reported that the convection can build global-scale magnetic fields that appear as wreaths of toroidal magnetic field of opposite polarity in each hemisphere These striking magnetic structures persist for long intervals despite being embedded within a turbulent convective layer. At a faster rotation rate of 5 , self-consistently generated magnetic wreaths at low latitudes underwent reversals in global magnetic polarity and cycles of magnetic activity (Brown et al, 2011) These cyclic reversals can be achieved at lower rotation rates if the diffusion is decreased, as the reversals can only occur when resistive diffusion is not able to prevent reversals in the axisymmetric poloidal fields (Nelson et al, 2013). Our work may be broadly applicable to processes occurring in the solar interior

Magnetism in Many Settings
Theoretical Approaches to Solar and Stellar Dynamos
Nature of the Simulation
Identifying Magnetic Loops
Properties of Rising Loops
Dynamics and Timing of Loop Ascents
Statistical Distribution of Twist and Tilt
Magnetic Cycles with Buoyant Loops
Relation of Loop Emergence and Mean Field Strength
Preferential Longitudes for Loop Creation
Findings
Summary and Reflections

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