THE SUN'S MERIDIONAL CIRCULATION AND INTERIOR MAGNETIC FIELD

To date, no self-consistent numerical simulation of the solar interior has succeeded in reproducing the observed thinness of the solar tachocline and the persistence of uniform rotation beneath it. Although it is known that the uniform rotation can be explained by the presence of a global-scale conf...

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Published inThe Astrophysical journal Vol. 738; no. 1; pp. 47 - jQuery1323904302645='48'
Main Authors WOOD, T. S, MCCASLIN, J. O, GARAUD, P
Format Journal Article
LanguageEnglish
Published Bristol IOP 01.09.2011
Subjects
Astronomy
ASTROPHYSICS, COSMOLOGY AND ASTRONOMY
COMPUTERIZED SIMULATION
Earth, ocean, space
Exact sciences and technology
FLUID MECHANICS
HYDRODYNAMICS
MAGNETIC FIELDS
MAGNETOHYDRODYNAMICS
MAIN SEQUENCE STARS
MECHANICS
MOTION
ROTATION
SIMULATION
STARS
SUN
Meridional flow
Magnetohydrodynamics
Sun: interior
Digital simulation
Sun: rotation
Sun
Convection
Persistence
MHD model
Magnetic fields
Diffusion
Solar interior
magnetohydrodynamics (MHD)
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Summary:To date, no self-consistent numerical simulation of the solar interior has succeeded in reproducing the observed thinness of the solar tachocline and the persistence of uniform rotation beneath it. Although it is known that the uniform rotation can be explained by the presence of a global-scale confined magnetic field, numerical simulations have thus far failed to produce any solution where such a field remains confined against outward diffusion. We argue that the problem lies in the choice of parameters for which these numerical simulations have been performed. We construct a simple analytical magnetohydrodynamic model of the solar interior and identify several distinct parameter regimes. For realistic solar parameter values, our results are in broad agreement with the tachocline model of Gough & McIntyre. In this regime, meridional flows driven at the base of the convection zone are of sufficient amplitude to hold back the interior magnetic field against diffusion. For the parameter values used in existing numerical simulations, on the other hand, we find that meridional flows are significantly weaker and, we argue, unable to confine the interior field. We propose a method for selecting parameter values in future numerical models.
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ISSN:0004-637X
1538-4357
DOI:10.1088/0004-637X/738/1/47