A simple method for determining the vertical growth rate of vertical motion at the top of earth's outer core

Physics

Scientific paper

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Scientific paper

A simple new method is described for extracting, from magnetic observations taken at Earth's surface, the vertical growth rate of vertical motion, ∂u/∂r, at special isolated points on the top surface of Earth's liquid core. The technique utilizes only the radial component of the frozen-flux induction equation and it requires information only on the radial magnetic field, Br, its horizontal gradient, and its secular variations, ∂Br/∂t, at the core-mantle boundary.

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