Geomagnetic/planetary dip poles at surface and magnetic fluxes at core-mantle boundary via satellite data

Computer Science

Scientific paper

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Scientific paper

Using 2001-2009 satellite data 728 consecutive Gaussian geomagnetic potential decompositions with degree n=10 were constructed. The dip poles on the surface and magnetic fluxes on core-mantle boundary were modeled with n from 1 till 10. Models with n about 7 are virtually indistinguishable with n=10 models, while magnetosphere and dynamo related integral properties start to converge at n=5 already. Some correspondent estimates are given for planets.

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