Issue |
A&A
Volume 508, Number 1, December II 2009
|
|
---|---|---|
Page(s) | 9 - 16 | |
Section | Astrophysical processes | |
DOI | https://doi.org/10.1051/0004-6361/200912614 | |
Published online | 08 October 2009 |
Online Material
Appendix A: Benchmarks for the code used
Here we present some benchmark tests for the computer code that we used and show how the crititical dynamo numbers and dynamo periods for the models of Sects. 3.1 and 3.2 converge for an increasing number of modes taken into account.
A.1 Free decay modes
First we test the accuracy of the implementation of the exterior boundary conditions
and the speed of convergence. If we neglect
all the dynamo effects in Eqs. (2) and (3), only simple isotropic
diffusion remains and the equations take the form
where for simplicity the magnetic diffusivity has been assumed to be homogeneous and has been set equal to unity. The equations for the poloidal and toroidal parts of the field are decoupled here. The eigenmodes to Eqs. (A.1) and (A.2) are the free decay modes, exponentially decaying


with
where the radial variable, x, varies in the interval
![$\left[0,1\right]$](/articles/aa/olm/2009/46/aa12614-09/img218.png)

The dependence of the solutions to Eqs. (A.1) and (A.2) on radius
is given analytically in terms of the spherical Bessel functions
(where Jn+1/2 is the ordinary Bessel function
of half-integer order n+1/2), and the decay rates,
,
are given by the squares of the zeros of the functions
jn-1 for the poloidal and jn for the toroidal modes.
The slowest decaying (largest scale) poloidal mode decays with the rate
,
the slowest decaying toroidal mode with the rate
;
the corresponding eigenfunctions are
and
.
These two decay modes are used for the test.
The
dependences of their potential functions
are given by the first terms (with m=1) in the latitudinal expansions
on the right-hand sides of Eqs. (A.3) and (A.4).
(The potential functions A and B differ from the potentials S and T in the
poloidal-toroidal decomposition
as normally used in non-axisymmetric cases,
see, e.g., Moffatt (1978) and Backus et al. (1996). For our axisymmetric case,
one has
and
.
The angular dependence of both S for the slowest decaying poloidal
mode and T for the slowest deacaying toroidal mode is given by
the spherical surface harmonic
,
in agreement with the
dependences of A and B as given above.)
Table A.1 shows the convergence of the eigenvalues and of
the corresponding eigenvectors for our numerical scheme.
Similar to Livermore & Jackson (2005), the eigenvectors
are scaled so that
and
,
and the errors are measured as
and
.
The number of modes in the radial basis, N,
is varied, while in the latitudinal basis just the first mode is taken
into account. The convergence is seen to be exponential in both the
poloidal and toroidal cases.
Table A.1:
Convergence of the eigenvalues and eigenvectors of the slowest decaying poloidal and toroidal modes.
A.2 Test case B of Jouve et al. (2008)
The next test case is taken from Jouve et al. (2008),
who presented a comparitative benchmark study of different numerical
codes for axisymmetric mean-field solar dynamo models in spherical
geometry. Here we consider their test case B, which is a pure
dynamo in a spherical shell with sharp gradients of the turbulent magnetic diffusivity and the strength of the
effect at the bottom of the convection zone; for details we refer to Jouve et al. (2008). The potential functions A and B are expanded according to Eqs. (21)-(26) in Sect. 2, and the integration domain is now radially bounded by
at the bottom and
at the top.
In Jouve et al. (2008), the strength of the
effect is regulated by a
dynamo number,
.
The different codes are compared by indicating in tables the critical
-effect dynamo number,
,
at which exponentially growing solutions appear, and the corresponding oscillation frequency,
.
In addition, butterfly diagrams and the evolution of the fields in the meridional plane are shown. Our values of
and
for different spectral resolutions are given in Table A.2,
and Fig. A.1
shows the temporal evolution of the toroidal and poloidal parts of the field
(i.e., of the unstable eigenmode) at the critical dynamo number.
The values in Table A.2 are in best agreement with those
given in the corresponding table, Table 3, of Jouve et al. (2008).
Similarly, the evolution shown in Fig. A.1 is apparently identical to that
shown in the corresponding figure, Fig. 7, of Jouve et al. (2008); the same applies to the simulated butterfly diagrams (not shown here).
![]() |
Figure A.1:
As Fig. 6 ( top and middle), but for test case B of Jouve et al. (2008) at the critical |
Open with DEXTER |
![]() |
Figure A.2:
Convergence of the critical dynamo numbers (left) and associated dynamo periods (right) for the models of Sects. 3.1 and 3.2. N is the total number of modes taken into account. Calculations were done for resolutions of |
Open with DEXTER |
Table A.2:
Test case B of Jouve et al. (2008).
A.3 Convergence of crititical dynamo numbers and dynamo periods for the models of Sects. 3.1 and 3.2
Figure A.2
shows the convergence of the critical dynamo numbers
(where the first dipolar mode becomes unstable) and associated dynamo periods for the
dynamo model considered in Sect. 3.1
and for the
dynamo model considered in Sect. 3.2.
The amplitude of the meridional flow is
and
;
is the value we used most, and
is the highest meridional-flow amplitude that we considered,
corresponding to the largest magnetic Reynolds number in the study.
High Reynolds numbers are known to cause numerical problems.
Appendix B: Definitions of the functions f
and f
Here we give the definitions of the functions fi(a) and fi(d) that are used in the representation of the turbulent electromotive force
.
For details of the calculations we refer to Pipin (2008).
![\begin{eqnarray*}f_{1}^{(a)} & = & \frac{1}
{4\Omega^{*~2}}\left[\left(\Omega^{*...
...^{*~2}+1\right)\frac{\arctan\Omega^{*}}
{\Omega^{*}}\right]\cdot
\end{eqnarray*}](/articles/aa/olm/2009/46/aa12614-09/img255.png)
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