A General Ocean Circulation Model Determined in a Simultaneous Solution with the Earth’s Gravity Field

  • R. Steven Nerem
  • Byron D. Tapley
  • C. K. Shum
Conference paper
Part of the International Association of Geodesy Symposia book series (IAG SYMPOSIA, volume 104)

Abstract

Over the past several years, determination of the sea surface topography using satellite altimetry has been greatly improved due to the implementation of a technique which simultaneously solves for the sea surface topography, the gravity field of the Earth, and the satellite orbit [Tapley et al.,1988; Marsh et al., 1989; Nerem,1989; Engelis and Knudsen; 1989]. The sea surface topography, ζ, is defined as the deviation of the ocean surface from the geoid due to the geostrophic component of the ocean currents.

Keywords

Covariance Geophysics Editing Aliasing Topex 

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Copyright information

© Springer-Verlag New York Inc. 1990

Authors and Affiliations

  • R. Steven Nerem
    • 1
  • Byron D. Tapley
    • 1
  • C. K. Shum
    • 1
  1. 1.Center for Space ResearchThe University of Texas at AustinAustinUSA

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