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EULAG-MHD: simulation of global solar dynamo
Piotr K Smolarkiewicz*, *National Center for Atmospheric Research, Boulder, Colorado, U.S.A.
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Toroidal component of B in the uppermost portion of the stable layer underlying the convective envelope at r/R≈
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Mihai Ghizaru, Paul Charbonneau, PK Smolarkiewicz, MAGNETIC CYCLES IN GLOBAL LARGE-EDDY SIMULATIONS OF SOLAR CONVECTION, The Astrophysical Journal Letters, 715:L133–L137, 2010; R. Bhattacharyya, B.C. Low, and P.K. Smolarkiewicz On spontaneous formation of current sheets: Untwisted magnetic fields. PHYSICS OF PLASMAS 17, Etienne Racine, P Charbonneau, M Ghizaru, Amelie Bouchat, PK Smolarkiewicz, ON THE MODE OF DYNAMO ACTION IN A GLOBAL LARGE-EDDY SIMULATION OF SOLAR CONVECTION, The Astrophysical Journal, 735:46 (22pp), 2011; Patrice Beaudoin, P. Charbonneau, E. Racine, P.K. Smolarkiewicz, Torsional Oscillations in a Global Solar Dynamo, Solar Physics (2012) in press Piotr K Smolarkiewicz, Paul Charbonneau EULAG, a Computational Model for Multiscale Flows: an MHD Extension Journal of Computational Physics, submitted
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Standard anelastic equations of solar magnetohydrodynamics
Brun, Miesch & Toomre,
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Elemental EULAG formulation
; Bauer, 1908
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Coordinate dependent form
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Coordinate dependent form
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Numerical approximations; background
elliptic problems for potentials
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Specialized MHD implementation
Hydrodynamic block
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Magnetic block Thermodynamics
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Model setups stable up to and unstable stable aloft
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Power of ILES
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Magnetic cycles
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Mode of large-scale dynamo action
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Remarks Notwithstanding some departures from the real solar climate, global MHD simulations of solar-like cycles have landed. EULAG-MHD offers an outstanding virtual MHD laboratory allowing to address quantitatively a number of questions that could until now only be speculated upon on the basis of simplified model formulations. There is much to be learned. For example, our calculations suggest that the entire magnetic variability involves less then 10% of solar luminosity connection to physics of other “dissipative structures” (QBO, MJO, ….) Numerics-wise we have learned that work of elliptic solvers is adaptive rather than additive
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Deriving the entropy equation
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What is A operator? Multidimensional positive definite advection transport algorithm (MPDATA):
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