The α effect with imposed and dynamo-generated magnetic fields

被引:23
|
作者
Hubbard, A. [1 ]
Del Sordo, F. [1 ,2 ]
Kapyla, P. J. [3 ]
Brandenburg, A. [1 ,2 ]
机构
[1] AlbaNova Univ Ctr, NORDITA, SE-10691 Stockholm, Sweden
[2] Stockholm Univ, Alba Nova Univ Ctr, Dept Astron, SE-10691 Stockholm, Sweden
[3] Univ Helsinki, Observ Tahtitorninmaki, FI-00014 Helsinki, Finland
基金
瑞典研究理事会; 欧洲研究理事会; 芬兰科学院;
关键词
hydrodynamics; magnetic fields; MHD; turbulence; LARGE-SCALE DYNAMOS; ROTATING MAGNETOCONVECTION; TURBULENT CONVECTION; OMEGA-DYNAMO; SIMULATIONS; ELECTRODYNAMICS; COEFFICIENTS; DIFFUSIVITY; GEODYNAMO; NUMBERS;
D O I
10.1111/j.1365-2966.2009.15108.x
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Estimates for the non-linear alpha effect in helical turbulence with an applied magnetic field are presented using two different approaches: the imposed-field method where the electromotive force owing to the applied field is used, and the test-field method where separate evolution equations are solved for a set of different test fields. Both approaches agree for stronger fields, but there are apparent discrepancies for weaker fields that can be explained by the influence of dynamo-generated magnetic fields on the scale of the domain that are referred to as meso-scale magnetic fields. Examples are discussed where these meso-scale fields can lead to both drastically overestimated and underestimated values of alpha compared with the kinematic case. It is demonstrated that the kinematic value can be recovered by resetting the fluctuating magnetic field to zero in regular time intervals. It is concluded that this is the preferred technique both for the imposed-field and the test-field methods.
引用
收藏
页码:1891 / 1899
页数:9
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