4.6 Article

Characterisation of the turbulent electromotive force and its magnetically-mediated quenching in a global EULAG-MHD simulation of solar convection

Journal

ADVANCES IN SPACE RESEARCH
Volume 58, Issue 8, Pages 1522-1537

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.asr.2016.03.041

Keywords

Magnetohydrodynamics; Solar cycle; Convection; Beta-effect; Diffusivity quenching

Funding

  1. Natural Sciences and Engineering Research Council of Canada
  2. Fond Quebecois pour la Recherche - Nature et Technologie
  3. Canadian Foundation for Innovation
  4. FRQNT/Quebec
  5. Calcul Quebec

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We perform a mean-field analysis of the EULAG-MHD millenium simulation of global magnetohydrodynamical convection presented in Passos and Charbonneau (2014). The turbulent electromotive force (emf) operating in the simulation is assumed to be linearly related to the cyclic axisymmetric, mean magnetic field and its first spatial derivatives. At every grid point in the simulation's meridional plane, this assumed relationship involves 27 independent tensorial coefficients. Expanding on Racine et al. (2011), we extract these coefficients from the simulation data through a least-squares minimization procedure based on singular value decomposition. The reconstructed alpha-tensor shows good agreement with that obtained by Racine et al. (2011), who did not include derivatives of the mean-field in their fit, as well as with the alpha-tensor extracted by Augustson et al. (2015) from a distinct ASH MHD simulation. The isotropic part of the turbulent magnetic diffusivity tensor beta is positive definite and reaches values of 5.0 x 10(7) m(2) s(-1) in the middle of the convecting fluid layers. The spatial variations of both alpha(phi phi) and beta(phi phi) component are well reproduced by expressions obtained under the Second Order Correlation Approximation, with a good matching of amplitude requiring a turbulent correlation time about five times smaller than the estimated turnover time of the small-scale turbulent flow. By segmenting the simulation data into epochs of magnetic cycle minima and maxima, we also measure alpha- and beta-quenching. We find the magnetic quenching of the alpha-effect to be driven primarily by a reduction of the small-scale flow's kinetic helicity, with variations of the current helicity playing a lesser role in most locations in the simulation domain. Our measurements of turbulent diffusivity quenching are restricted to the beta(phi phi) component, but indicate a weaker quenching, by a factor of similar or equal to 1.36, than of the alpha-effect, which in our simulation drops by a factor of three between the minimum and maximum phases of the magnetic cycle. (C) 2016 COSPAR. Published by Elsevier Ltd. All rights reserved.

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