P. J. Käpylä, M. J. Mantere, A. Brandenburg
We present results from compressible Cartesian convection simulations with
and without imposed shear. In the former case the dynamo is expected to be of
alpha^2 Omega type which is likely to be relevant for the Sun, whereas the
latter case refers to alpha^2 dynamos which are more likely to occur in more
rapidly rotating stars. The latter exhibit oscillatory large-scale magnetic
fields. We perform a parameter study where the shear flow is kept fixed and the
rotational influence is varied in order to probe the relative importance of
both modes. We find that in cases with shear, the streamwise component of the
magnetic field is between 9 and 20 times greater than the cross-streamwise one,
depending on the rotation rate. Oscillatory solutions are preferred either when
the shear is relatively strong or weak in comparison to rotation, but not when
the two are comparable to each other. However, exceptions to these rules also
appear and in many cases the solution is oscillatory only in the kinematic
regime whereas in the nonlinear stage the mean fields are stationary. The cases
with rotation and no shear are always oscillatory in the parameter range
studied here and the dynamo mode does not depend on the magnetic boundary
conditions. The strength of total and the large-scale component of the magnetic
field at the saturated state, however, are sensitive to the chosen boundary
conditions.
View original:
http://arxiv.org/abs/1111.6894
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