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We present a new model of the radial (1-D) conductivity structure of Earth&#39;s mantle. This model is derived from more than 10yr of magnetic measurements from the satellites Ørsted, CHAMP, SAC-C and the Swarm trio as well as the global network of geomagnetic observatories. After removal of core and crustal field as predicted by a recent field model, we fit the magnetic data with spherical harmonic ...

A new model of Earth's radial conductivity structure derived from over 10 yr of satellite and observatory magnetic data