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UK MHD Meeting 2004 

Thursday 6th and Friday 7th May 2004

Nice - Cote D'Azur

Laboratory Cassiopée UMR6202 CNRS 
Observatory of the Cote d'Azur

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Quasi-geostrophic dynamos

Nathanael Schaeffer  ,  LGIT Grenoble

Taking advantage of the properties of liquid metals and of rapidly rotating
flows, we are able to compute dynamos at high Reynolds number (Re > 100 000)
and low magnetic Prandtl number (Pm < 0.01)

We developped a numerical model that uses a quasi-goestrophic approximation
to compute the flow (whithout subgrid scale model), leading to two-dimensional equations.
The induction equation for the magnetic field is fully resolved in 3D, in a sphere.
This approach proves quite efficient for low magnetic Prandtl number and
suitable flows, for which there is a scale separation between magnetic field and
velocity field, allowing to compute the magnetic field on a coarser grid and whith
larger time steps than for the velocity field.
We show results of these calculations applied on the turbulent flow produced by
the destabilization of a Stewartson shear layer.


   

 
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