Nathanaël Schaeffer

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The contribution of small scale turbulent fluctuations to the induction of a mean magnetic field is investigated in our liquid sodium spherical Couette experiment with an imposed magnetic field. An inversion technique is applied to a large number of measurements at Rm≈100 to obtain radial profiles of the α and β effects and maps of the mean flow. It appears(More)
We present a reconstruction of the mean axisymmetric azimuthal and meridional flows in the Derviche Tourneur Sodium installation in Grenoble liquid sodium experiment. The experimental device sets a spherical Couette flow enclosed between two concentric spherical shells where the inner sphere holds a strong dipolar magnet, which acts as a magnetic propeller(More)
Torsional Alfvén waves propagating in the Earth's core have been inferred by inversion techniques applied to geomagnetic models. They appear to propagate across the core but vanish at the equator, exchanging angular momentum between core and mantle. Assuming axial symmetry, we find that an electrically conducting layer at the bottom of the mantle can lead(More)
We present a dynamo mechanism arising from the presence of barotrop-ically unstable zonal jet currents in a rotating spherical shell. The shear instability of the zonal flow develops in the form of a global Rossby mode, whose azimuthal wavenumber depends on the width of the zonal jets. We obtain self-sustained magnetic fields at magnetic Reynolds numbers(More)
Sujet: La génération du champ magnétique des planètes (Terre, Jupiter, Saturne, Neptune, …) repose sur le mécanisme dynamo qui produit un champ magnétique par les mouvements d'un fluide conducteur. Des expériences ont reproduit ce phénomène, mais les dynamos des planètes ont des spécificités particulières (dipolarité, rôle important du champ magnétique dans(More)
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