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Monitoring Geoidal Potential on the Basis of Topex/Poseidon Altimeter Data and EGM96

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Geodesy on the Move

Part of the book series: International Association of Geodesy Symposia ((IAG SYMPOSIA,volume 119))

Abstract

The geopotential scale factor R 0 = GM/W 0 (GM — the adopted gravitational constant) and/or geoidal potential W 0 have been determined from the EGM96 geopotential model, the POCM 4B sea surface topography model and three years (1994–1996) of TOPEX POSEIDON (T/P) altimetry data: R 0 = (6 363 672.589 ±0.050) m; W 0 = (62 636 855.72 ±0.50) m2 s2. The 5 cm uncertainty in altimetry calibration limits the actual accuracy of the solution. However, the formal rms of R 0 is less than ±1mm which makes the monitoring W 0 and R 0 promising. Continuous W 0 /R 0 monitoring has been initiated in early 1997 and monthly values of W 0 and R 0 are presented and discussed.

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© 1998 Springer-Verlag Berlin Heidelberg

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Burša, M., Kouba, J., Raděj, K., True, S.A., Vatrt, V., Vojtíšková, M. (1998). Monitoring Geoidal Potential on the Basis of Topex/Poseidon Altimeter Data and EGM96. In: Forsberg, R., Feissel, M., Dietrich, R. (eds) Geodesy on the Move. International Association of Geodesy Symposia, vol 119. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-72245-5_55

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  • DOI: https://doi.org/10.1007/978-3-642-72245-5_55

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-72247-9

  • Online ISBN: 978-3-642-72245-5

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