The earth's C21 and S21 gravity coefficients and the rotation of the core.

Physics

Scientific paper

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Earth Core:Rotation, Earth:Gravitation, Gravitation:Earth, Rotation:Earth Core

Scientific paper

Observational results for the earth's C21 and S21 gravity coefficients can be used to constrain the mean equatorial rotation of the core with respect to the mantle. Current satellite gravity solutions suggest the equatorial rotation rate is no larger than 1×10-7times the earth's diurnal spin rate, a limit more than one order of magnitude smaller than the polar rotation rate inferred from the westward drift of the earth's magnetic field.

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