The flow within the Earth created by the relative rotation of the mantle and solid core.

Details The flow within the Earth created by the relative rotation of the mantle and solid core. The flow within the Earth created by the relative rotation of the mantle and solid core.

Aug 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990ge%26ae..30...99n&link_type=abstract

Geomagn. Aeron., Vol. 30, No. 1, p. 99 - 102

Physics

Fluid Dynamics

Earth Core: Fluid Dynamics

Scientific paper

A large-scale flow, including differential rotation and meridional circulation, arises in the liquid density-stratified outer core as a result of the difference in angular velocities between the mantle and solid core. The steady-state difference in angular velocities is maintained by a balance between the moments of the external (tidal) forces and the internal viscous and magnetic friction.

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