Rapid diffusion of the poloidal geomagnetic field through the weakly conducting mantle: a perturbation solution.

Details Rapid diffusion of the poloidal geomagnetic field through the weakly conducting mantle: a perturbation solution. Rapid diffusion of the poloidal geomagnetic field through the weakly conducting mantle: a perturbation solution.

Oct 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983geoji..75...77b&link_type=abstract

Geophysical Journal International, Vol. 75, No. 1, p. 77 - 100

Physics

6

Geomagnetic Field:Models

Scientific paper

A systematic regular perturbation procedure is developed to account for
weak mantle conduction as unsteady electromagnetic fields are
extrapolated downward from the Earth's surface to the core-mantle
boundary.

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