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High resolution analysis of satellite gradiometrySatellite gravity gradiometry is a technique now under development which, by the middle of the next decade, may be used for the high resolution charting from space of the gravity field of the earth and, afterwards, of other planets. Some data analysis schemes are reviewed for getting detailed gravity maps from gradiometry on both a global and a local basis. It also presents estimates of the likely accuracies of such maps, in terms of normalized spherical harmonics expansions, both using gradiometry alone and in combination with data from a Global Positioning System (GPS) receiver carried on the same spacecraft. It compares these accuracies with those of current and future maps obtained from other data (conventional tracking, satellite-satellite tracking, etc.), and also with the spectra of various signals of geophysical interest.
Document ID
19900011245
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Colombo, O. L.
(EG and G Washington Analytical Services Center, Inc. Lanham, UT, United States)
Date Acquired
September 6, 2013
Publication Date
June 1, 1989
Publication Information
Publication: Ohio State Univ., Progress in the Determination of the Earth's Gravity Field
Subject Category
Geophysics
Accession Number
90N20561
Funding Number(s)
CONTRACT_GRANT: NAS5-28067
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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