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Undulation and anomaly estimation using Geos-3 altimeter data without precise satellite orbits
Abstract The paper describes results obtained from the processing of 53 Geos-3 arcs of altimeter data obtained during the first weeks after the launch of the satellite in April, 1975. The measurement from the satellite to the ocean surface was used to obtain an approximate geoid undulation which was contaminated by long wavelength errors caused primarily by altimeter bias and orbit error. This long wavelength error was reduced by fitting with a low degree polynomial the raw undulation data to the undulations implied by the GEM 7 potential coefficients, in an adjustment process that included conditions on tracks that cross. The root mean square crossover discrepancy before this adjustment was ±12.4 meters while after the adjustment it was ±0.9 m. These adjusted undulations were used to construct a geoid map in the Geos-3 calibration area using a least squares filter to remove remaining noise in the undulations. Comparing these undulations to ones computed from potential coefficients and terrestrial gravity data indicates a mean difference of 0.25 m and a root mean square difference of ±1.92 m. The adjusted undulations were also used to estimate several $ 5^{o} $, $ 2^{o} $, and $ 1^{o} $ anomalies using the method of least squares collocation. The resulting predictions agreed well with known values although the $ 1^{o} $ x $ 1^{o} $ anomalies could not be considered as reliably determined.
Undulation and anomaly estimation using Geos-3 altimeter data without precise satellite orbits
Abstract The paper describes results obtained from the processing of 53 Geos-3 arcs of altimeter data obtained during the first weeks after the launch of the satellite in April, 1975. The measurement from the satellite to the ocean surface was used to obtain an approximate geoid undulation which was contaminated by long wavelength errors caused primarily by altimeter bias and orbit error. This long wavelength error was reduced by fitting with a low degree polynomial the raw undulation data to the undulations implied by the GEM 7 potential coefficients, in an adjustment process that included conditions on tracks that cross. The root mean square crossover discrepancy before this adjustment was ±12.4 meters while after the adjustment it was ±0.9 m. These adjusted undulations were used to construct a geoid map in the Geos-3 calibration area using a least squares filter to remove remaining noise in the undulations. Comparing these undulations to ones computed from potential coefficients and terrestrial gravity data indicates a mean difference of 0.25 m and a root mean square difference of ±1.92 m. The adjusted undulations were also used to estimate several $ 5^{o} $, $ 2^{o} $, and $ 1^{o} $ anomalies using the method of least squares collocation. The resulting predictions agreed well with known values although the $ 1^{o} $ x $ 1^{o} $ anomalies could not be considered as reliably determined.
Undulation and anomaly estimation using Geos-3 altimeter data without precise satellite orbits
Rummel, R. (author) / Rapp, R. H. (author)
Bulletin Géodésique ; 51
1977
Article (Journal)
Electronic Resource
English
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