Geodetic Features of the Ocean Surface and Their Implications 1984
DOI: 10.1007/978-94-017-1673-4_5
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Field Tests of SEASAT Bathymetric Detections

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Cited by 2 publications
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“…The geoid represents the gravitational equipotential surface of the Earth relative to the mean sea level; gravity varies in space, and the anomalies in its distribution were found to be correlated with bathymetry (McKenzie and Bowin, 1976;Watts 1979). Despite initial reports stating that it was impossible to derive reliable bathymetry from satellite altimeter (Keating et al, 1984;Watts and Ribe, 1984), Dixon et al (1983) were the first to demonstrate its feasibility using real data. Several algorithms and methods to estimate and predict bathymetry from the gravitational field have since been developed (reviewed in Calmant andBeaudry, 1996 andSmith, 2001).…”
Section: Satellite Radar Altimetrymentioning
confidence: 99%
“…The geoid represents the gravitational equipotential surface of the Earth relative to the mean sea level; gravity varies in space, and the anomalies in its distribution were found to be correlated with bathymetry (McKenzie and Bowin, 1976;Watts 1979). Despite initial reports stating that it was impossible to derive reliable bathymetry from satellite altimeter (Keating et al, 1984;Watts and Ribe, 1984), Dixon et al (1983) were the first to demonstrate its feasibility using real data. Several algorithms and methods to estimate and predict bathymetry from the gravitational field have since been developed (reviewed in Calmant andBeaudry, 1996 andSmith, 2001).…”
Section: Satellite Radar Altimetrymentioning
confidence: 99%