RSGEC Gravimetric Geodesy

Earth’s shape and gravity are intimately associated. Gravimetric geodesy is based on the strength variety of a gravitational field to gain parameters such as equipotential surfaces, then we have geoid which can be used to measure significant wave of sea, tidal load. Similarly, applied to measuring the variety of groundwater storage according to local mass change. Morden gravimetric geodesy mainly relies on satellites.