GRACE: Gravity Recovery and Climate Experiment Brochure [PDF]
This brochure provides details about NASA's GRACE mission. Gravity controls everything from the motion of the ocean tides to the expansion of the entire Universe.
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On the Consistency between a Classical Definition of the Geoid-to-Quasigeoid Separation and Helmert Orthometric Heights. [PDF]
Tenzer R, Nsiah Ababio A.
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Upper mantle heterogeneity: Comparisons of regions south of Australia with Philippine Basin [PDF]
The nature of mass anomalies that occur beneath the regions of negative residual depth anomalies were identified. Residual geoid anomalies with negative residual depth anomalies are identified in the Philippine Basin (negative) and in the region south of
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Global detailed gravimetric geoid [PDF]
A global detailed gravimetric geoid has been computed by combining the Goddard Space Flight Center GEM-4 gravity model derived from satellite and surface gravity data and surface 1 deg-by-1 deg mean free air gravity anomaly data.
Marsh, J. G., Vincent, S.
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Strategies for estimating the marine geoid from altimeter data [PDF]
Altimeter 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 ...
Argentiero, P. +2 more
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Sea floor swells and mantle plumes [PDF]
Most of the intraplate oceanic hot spots are located on the crest of broad topographic swells in the sea floor. These swells have Gaussian shaped profiles, with up to 1.6 km of relief and half widths of 200 to 300 km.
Olson, P.
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Short arc reduction of radar altimetry computer program [PDF]
The Air Force Geophysics Laboratory computer program SARRA (Short Arc Reduction of Radar Altimetry) has been used for geoid determination with altimetric observations from the GEOS-3 satellite.
Hadgigeorge, G., Trotter, J.
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The application of Skylab altimetry to marine geoid determination [PDF]
The author had identified the following significant results. The major results can be divided broadly into two groups. One group is concerned with the effects of errors inherent in the various input data, such as the orbit emphemeris, a priori geoid etc.
Fubara, D. M. +3 more
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Reprocessed precise science orbits and gravity field recovery for the entire GOCE mission. [PDF]
Arnold D +4 more
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Geoid undulations and gravity anomalies over the Aral Sea, the Black Sea and the Caspian Sea from a combined GEOS-3/SEASAT/GEOSAT altimeter data set [PDF]
Satellite-based altimetric data taken by GOES-3, SEASAT, and GEOSAT over the Aral Sea, the Black Sea, and the Caspian Sea are analyzed and a least squares collocation technique is used to predict the geoid undulations on a 0.25x0.25 deg.
Au, Andrew Y. +2 more
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