CMB topography deforms geostrophic contours, enabling buoyancy to strengthen outer-core convection and produce torques consistent with observed decadal LOD variations.
A., Noir, J., Eldredge, J
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Effects of global core-mantle boundary topography on outer-core convection and topographic torques
CMB topography deforms geostrophic contours, enabling buoyancy to strengthen outer-core convection and produce torques consistent with observed decadal LOD variations.