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Chapter
CHAMP Gravity Anomalies over Antarctica
Before CHAMP, the Antarctic gravity field was constrained predominantly by satellite altimetry-derived gravity measurements over the oceans and the variations in satellite orbits at altitudes of about 700 km a...
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Chapter and Conference Paper
The TEG-3 Geopotential Model
A new solution for the static geopotential, TEG-3, complete to 70×70 in spherical harmonics, has been obtained. The solution represents one of the latest efforts to improve the Earth’s gravity model. The solut...