Similar to Fig.K.1, but comparing the torque of the hemispherical ocean model between a pure oceanic response, and the response of the ocean when accounting for loading and self-attraction effects arising from solid Earth deformation assuming an Andrade rheology. The procedure of this coupling for the hemispheric configuration is detailed in Appendix F. We recall that the energy tidally dissipated in the solid part is ignored in the hemispherical configuration.