Physics – Fluid Dynamics
Scientific paper
Dec 1989
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989gapfd..49..195s&link_type=abstract
Geophysical and Astrophysical Fluid Dynamics, Vol. 49, No. 1-4, p. 195 - 211
Physics
Fluid Dynamics
4
Dynamo Theory: Earth Core
Scientific paper
The linear hydromagnetic stability problem for a horizontal non-constantly stratified fluid layer rapidly rotating about the z-axis and permeated by an azimuthal non-homogeneous magnetic field is investigated. A non-linear (parabolic) temperature profile is used to simulate the lower part of the fluid core being unstably stratified and the upper part stably stratified. The problem is solved on the magnetic diffusion timescale and for q < 1 (q is the ratio of the thermal and magnetic diffusivities). The model is investigated for various widths of the stably stratified part of the layer and for a wide range of values of the azimuthal magnetic strength.
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