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Degradation of Geopotential Recovery from Short Repeat-Cycle Orbits: Application to GRACE Monthly Fields

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Abstract

Throughout 2004 the GRACE (Gravity Recovery And Climate Experiment) orbit contracted slowly to yield a sparse repeat track of 61 revolutions every 4 days on 19 September 2004. As a result, we show from linear perturbation theory that geopotential information previously available to fully resolve a gravity field every month of 120× 120 (degree by order) in spherical harmonics was compressed then into about one-fourth of the necessary observation space. We estimate from this theory that the ideal gravity field resolution in September 2004 was only about 30 × 30. More generally, we show that any repeat-cycle mission for geopotential recovery with full resolution L × L requires the number of orbit-revolutions-to-repeat to be greater than 2L.

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References

  • Bettadpur S (2004) GRACE mission status and gravity field product improvement plans. Eos Trans AGU 85(47), Fall meet. Suppl., Abstract G23A-01

  • Colombo O (1984) Altimetry, orbits and tides, NASA Tech. Memo. 86180. Goddard Space Flight Center, Greenbelt, 173 pp

  • Han S, Shum C, Braun A (2005) High-resolution continental water storage recovery from low–low satellite-to-satellite tracking. J Geodyn 39:11–28

    Article  Google Scholar 

  • Kaula W (1966) Theory of satellite geodesy. Blaisdell Press, Waltham, 134 pp

    Google Scholar 

  • Press W, Flannery B, Teukolsky S, Vettering W (1987) Numerical recipes: the art of scientific computing. Cambridge University Press, Cambridge

    Google Scholar 

  • Tapley B, Bettadpur S, Watkins M, Reigber Ch (2004) The gravity recovery and climate experiment: mission overview and early results. Geophys Res Lett 31: L09607. DOI 10.1029/2004GL019920

    Article  Google Scholar 

  • Wagner C (1987) Improved gravitational recovery from a geopotential research mission satellite pair flying en-echelon. J Geophys Res 92(B8):8147–8155

    Article  Google Scholar 

  • Wagner C (1991) A prograde geosat exact repeat mission. J Astronaut. Sci 39(3):316–326

    Google Scholar 

  • Wagner C, McAdoo D (2004) Time variations in the GRACE gravity field: constraints on global hydrologic mass flux. In: Reigber C, Tapley B (eds) Proceedings of the joint CHAMP/GRACE science meeting, GFZ Potsdam, 6–8 July

  • Wahr J, Swenson S, Zlotnicki V, Velicogna I (2004) Time variable gravity from GRACE: first results. Geophys Res Lett 31: L11501. DOI 10.1029/2004GL019779

    Article  Google Scholar 

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Correspondence to C. Wagner.

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Wagner, C., McAdoo, D., Klokočník, J. et al. Degradation of Geopotential Recovery from Short Repeat-Cycle Orbits: Application to GRACE Monthly Fields. J Geodesy 80, 94–103 (2006). https://doi.org/10.1007/s00190-006-0036-x

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  • DOI: https://doi.org/10.1007/s00190-006-0036-x

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