The electric field produced in the mantle by the dynamo in the core
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference39 articles.
1. Riemann Surfaces;Ahlfors,1960
2. A class of self-sustaining dissipative spherical dynamos;Backus;Ann. Phys.,1958
3. Potentials for tangent tensor fields on spheroids;Backus;Arch. Ration. Mech. Anal.,1966
4. Kinematics of geomagnetic secular variation in a perfectly conducting core;Backus;Philos. Trans. R. Soc. London,1968
5. An L2 form of Bernstein's inequality;Backus;Proc. Natl. Acad. Sci. USA,1979
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1. Secular variation of the poloidal magnetic field at the core-mantle boundary;Geophysical Journal International;2002-02-27
2. Constraining electromagnetic core–mantle coupling;Physics of the Earth and Planetary Interiors;1999-02
3. Time-varying fluid flow at the top of Earth's core derived from definitive geomagnetic reference field models;Journal of Geophysical Research: Solid Earth;1995-06-10
4. Electromagnetic Coupling and the Toroidal Magnetic Field At the Core-Mantle Boundary;Geophysical Journal International;1994-04
5. Simultaneous solution for core magnetic field and fluid flow beneath an electrically conducting mantle;Journal of Geophysical Research;1994
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