Physics
Scientist
GeoForschungsZentrum Potsdam, Department 1: Geodesy and Remote Sensing, Telegrafenberg, D-14473, Potsdam, Germany
Displacement of Martian Surface Due to Seasonal Surface Mass Redistribution and Its Detection from Lander-Orbiter-Earth Radio Links
Geoid displacement about Greenland resulting from past and present-day mass changes in the Greenland Ice Sheet
Time-domain approach to linearized rotational response of a three-dimensional viscoelastic earth model induced by glacial-isostatic adjustment: I. Inertia-tensor perturbations
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