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Application of Satellite Radar Altimeter Data to the Determination of Regional Tidal Constituents and the Mean Sea Surface

  • John M. Diamante
  • Tsun-Shi Nee
Part of the Marine Science book series (MR, volume 13)

Abstract

A method has been developed to correct the systematic satellite ephemeris errors in satellite radar altimeter data over an extended extrapolation area, having first determined these errors in a reference region where an accurate gravimetric geoid and tide model are available.

The method has been applied using GEOS-3 altimeter data in the GEOS-3 Atlantic Ocean Calibration Area, using a portion of the Hatteras Abyssal Plain as the reference area, to derive the mean sea surface and five tidal constituents in the extrapolation region.

Keywords

Reference Region Reference Area Altimeter Data Tide Model Tidal Constituent 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Cartwright, D., Zetler, B. and Hamon, B., 1979, “Pelagic Tidal Constituents,” lAPSO Publication Scientifique No. 30, IAPSO Advisory Committee on Tides and Mean Sea Level.Google Scholar
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  4. Maul, G. and Yanaway, A., 1978, “Deep Sea Tides Determination from GEOS-3,” NASA Contractor Report 141435, National Aeronautics and Space Administration, Wallops Flight Center, Wallops Flight Center, Wallops Island, VA.Google Scholar
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  6. Mofjeld, H.O., 1975, “Empirical Model for Tides in the Western 918 North Atlantic Ocean,” NOAA Technical Report ERL 340-AOML 19, U.S. Department of Commerce, National Oceanic and Atmospheric Administration, Boulder, Co.Google Scholar

Copyright information

© Plenum Press, New York 1981

Authors and Affiliations

  • John M. Diamante
    • 1
  • Tsun-Shi Nee
    • 2
  1. 1.NOAA/National Ocean SurveyRockvilleUSA
  2. 2.Optimum Systems, IncRockvilleUSA

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