Electromagnetic coupling and the toroidal magnetic field at the core-mantle boundary.

Details Electromagnetic coupling and the toroidal magnetic field at the core-mantle boundary. Electromagnetic coupling and the toroidal magnetic field at the core-mantle boundary.

Apr 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994geoji.117..235l&link_type=abstract

Geophysical Journal International, Vol. 117, No. 1, p. 235 - 256

Physics

17

Earth Rotation: Variations

Scientific paper

Owing to exchanges of angulur momentum between the Earth's fluid outer core and the overlying solid mantle, the Earth's rotational rate fluctuates on periods of a few years to a few decades. However, the mechanism which allows the exchange of angular momentum is not understood. Here the authors examine the possibility that core-mantle coupling is predominantly electromagnetic and thus responsible for the decadal length of day variations.

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