Towards a standard model of present-day signals due to post-glacial rebound

I am currently in the process of intercomparing these predictions as well as comparing them to geodetic observations.

One test is the inclusion of the PGS signal in the determination of the rigid plate motion for the main tectonic plates from GPS-observed secular velocities. These results were reported in a poster at the annual meeting of the European Geoscience Union (EGU) in Vienna, 2005. The poster is available here.