On the nearly axially-symmetrical model of the hydromagnetic dynamo of the earth

Details On the nearly axially-symmetrical model of the hydromagnetic dynamo of the earth On the nearly axially-symmetrical model of the hydromagnetic dynamo of the earth

Jan 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976pepi...11..191b&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 11, Issue 3, p. 191-199.

Physics

15

Scientific paper

A short review of the present state of the nearly axially-symmetrical dynamo model is given. A simplified theory for hydromagnetic dynamos taking into account the forces acting in the Earth's core is considered. The role of weak core-mantle friction is discussed and a form of solution is suggested which is characterized by a large geostrophic velocity in the core and by a boundary layer of a new type. The consequences of such a model (called model Z) for the Earth's dynamo are discussed.

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