Accuracy of Mean Earth Ellipsoid Based on Doppler, Laser, and Altimeter Observations.

Abstract

The error in the mean earth ellipsoid computed on the basis of Doppler or laser observations of artificial earth satellites or radar altimeter observations of the ocean surface from a satellite depends upon instrument precision, on uncertainties in the specification of the earth's gravity field at both long and short wavelengths, on uncertainties in the origin of the coordinate system, on modeling errors in ionospheric (except laser) and tropospheric refraction, and, for altimetry, on oceanographic effects. The magnitude of the uncertainty in the computed ellipsoid will vary, depending on the size of these errors and on the number and distribution of observation stations. Review of computations based on various data sets indicates that differences in the computed ellipsoids are consistent with those expected, due to the various error sources and that the best-fitting ellipsoid has a semimajor axis of 6378136 + or - 2 m. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1980
Accession Number
ADA081966

Entities

People

  • Richard J. Anderle

Organizations

  • Naval Surface Warfare Center Dahlgren Division

Tags

Communities of Interest

  • Space

DTIC Thesaurus Topics

  • Accuracy
  • Altimeters
  • Altimetry
  • Artificial Satellites
  • Assembly
  • Coordinate Systems
  • Data Sets
  • Ephemerides
  • Ground Stations
  • Long Wavelengths
  • Satellite Antennas
  • Satellite Orbits
  • Short Wavelengths
  • Standards
  • Stations
  • Uncertainty
  • United States

Fields of Study

  • Environmental science

Readers

  • Regression Analysis.
  • Space Exploration and Orbital Mechanics.

Technology Areas

  • Directed Energy
  • Space
  • Space - Orbital Debris