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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...

    Ralph R. B. von Frese, Laramie V. Potts in First CHAMP Mission Results for Gravity, M… (2003)

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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...

    B. D. Tapley, C. K. Shum, J. C. Ries, S. R. Poole in Gravity, Geoid and Marine Geodesy (1997)