Shallow Earth Rheology from Glacial Isostatic Adjustment Constrained by GOCE

High-harmonic geoid signatures related to glacial isostatic adjustment and their detectability by GOCE

Shallow-Earth Rheology from Glacial Isostasy and Satellite Gravity, a sensitivity analysis for GOCE

Postglacial induced surface motions, sea-levels and geoid rates on a spherical, self-gravitating laterally heterogeneous Earth

Sentitivity of glacial isostatic adjustment models with shallow low-viscosity earth layers to the ice-load history in relation to the performance of GOCE and GRACE

High-harmonic geoid signatures due to glacial isostatic adjustment, subduction and seismic deformation