Am. Forte et al., SEISMIC-GEODYNAMIC DETERMINATION OF THE ORIGIN OF EXCESS ELLIPTICITY OF THE CORE-MANTLE BOUNDARY, Geophysical research letters, 22(9), 1995, pp. 1013-1016
We demonstrate that the excess dynamic ellipticity of the core-mantle-
boundary (CMB) inferred from the period of the Earth's retrograde free
core nutation (RFCN) may be explained in terms of viscous stresses ge
nerated by mantle convective flow. The 3D elastic structure and radial
viscosity profile which define the model used in the viscous flow cal
culations are;constrained to simultaneously reconcile a large set of s
eismic and geodynamic data.