Add to ORKGAltimeter data from a spacecraft borne altimeter was processed to estimate the fine structure of the marine geoid. Simulation studies show that, among several competing parameterizations, the mean free air gravity anomaly model exhibited promising geoid recovery characteristics. Using covariance analysis techniques, quantitative measures of the orthogonality properties are investigated
The Skylab Altimeter Experiment has proven the capability of the altimeter for measurement of sea su...
An optimal procedure is developed for deriving gravity anomalies from sea-surface height measurement...
A model for the recovery of gravity anomalies from high precision altimeter data is derived which co...
In processing altimeter data from a spacecraft borne altimeter to estimate the fine structure of the...
Gravity anomalies have been recovered in the North Atlantic and the Indian Ocean regions. Comparison...
A number of detailed gravimetric geoids of portions of the world's oceans from marine gravity measur...
The accuracy with which the local ocean geoid structure could be determined using satellite altimetr...
Progress in the following areas is described: refining altimeter and altimeter crossover measurement...
Data from spacecraft altimeters are expected to contribute to an improved determination of the marin...
The author had identified the following significant results. The major results can be divided broadl...
The GEOS-C spacecraft is scheduled to carry onboard a radar altimeter for the purpose of measuring t...
The characteristics of the geoid surface are quantitatively described. A procedure for calculating t...
Marine geoid is crucial for orthometric height determination. The airborne and shipborne surveys hav...
A technique for deriving mean gravity anomalies from dense altimetry data was developed. A combinati...
Two methods are tested whereby satellite altimeter measurements of the geoid height are combined wit...
The Skylab Altimeter Experiment has proven the capability of the altimeter for measurement of sea su...
An optimal procedure is developed for deriving gravity anomalies from sea-surface height measurement...
A model for the recovery of gravity anomalies from high precision altimeter data is derived which co...
In processing altimeter data from a spacecraft borne altimeter to estimate the fine structure of the...
Gravity anomalies have been recovered in the North Atlantic and the Indian Ocean regions. Comparison...
A number of detailed gravimetric geoids of portions of the world's oceans from marine gravity measur...
The accuracy with which the local ocean geoid structure could be determined using satellite altimetr...
Progress in the following areas is described: refining altimeter and altimeter crossover measurement...
Data from spacecraft altimeters are expected to contribute to an improved determination of the marin...
The author had identified the following significant results. The major results can be divided broadl...
The GEOS-C spacecraft is scheduled to carry onboard a radar altimeter for the purpose of measuring t...
The characteristics of the geoid surface are quantitatively described. A procedure for calculating t...
Marine geoid is crucial for orthometric height determination. The airborne and shipborne surveys hav...
A technique for deriving mean gravity anomalies from dense altimetry data was developed. A combinati...
Two methods are tested whereby satellite altimeter measurements of the geoid height are combined wit...
The Skylab Altimeter Experiment has proven the capability of the altimeter for measurement of sea su...
An optimal procedure is developed for deriving gravity anomalies from sea-surface height measurement...
A model for the recovery of gravity anomalies from high precision altimeter data is derived which co...