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Recent first principles calculations of the Earth&#39;s outer core thermal and electrical conductivities have raised their values by a factor of three. This has significant implications for geodynamo operation, in particular, forcing the development of a stably stratified layer at the core–mantle boundary (CMB). This study seeks to test the hypothesis of a stably stratified layer in the uppermost core...

Are geomagnetic data consistent with stably stratified flow at the core–mantle boundary?