A platform for research: civil engineering, architecture and urbanism
Gravity anomalies from satellite altimetry: comparison between computation via geoid heights and via deflections of the vertical
Abstract The accumulation of good quality satellite altimetry missions allows us to have a precise geoid with fair resolution and to compute free air gravity anomalies easily by fast Fourier transform (FFT) techniques. In this study we are comparing two methods to get gravity anomalies. The first one is to establish a geoid grid and transform it into anomalies using inverse Stokes formula in the spectral domain via FFT. The second one computes deflection of the vertical grids and transforms them into anomalies. The comparison is made using different data sets: Geosat, ERS-1 and Topex-Poseidon exact repeat misions (ERMs) north of 30°S and Geosat geodetic mission (GM) south of 30°S. The second method which transforms the geoid gradients converted into deflection of the vertical values is much better and the results have been favourably evaluated by comparison with marine gravity data.
Gravity anomalies from satellite altimetry: comparison between computation via geoid heights and via deflections of the vertical
Abstract The accumulation of good quality satellite altimetry missions allows us to have a precise geoid with fair resolution and to compute free air gravity anomalies easily by fast Fourier transform (FFT) techniques. In this study we are comparing two methods to get gravity anomalies. The first one is to establish a geoid grid and transform it into anomalies using inverse Stokes formula in the spectral domain via FFT. The second one computes deflection of the vertical grids and transforms them into anomalies. The comparison is made using different data sets: Geosat, ERS-1 and Topex-Poseidon exact repeat misions (ERMs) north of 30°S and Geosat geodetic mission (GM) south of 30°S. The second method which transforms the geoid gradients converted into deflection of the vertical values is much better and the results have been favourably evaluated by comparison with marine gravity data.
Gravity anomalies from satellite altimetry: comparison between computation via geoid heights and via deflections of the vertical
Olgiati, A. (author) / Balmino, G. (author) / Sarrailh, M. (author) / Green, C. M. (author)
Bulletin géodésique ; 69
1995
Article (Journal)
English
Geodäsie , Geometrie , Geodynamik , Zeitschrift , Mathematik , Mineralogie
Deflections of the vertical and geoid heights from gravity gradients
Online Contents | 2005
|Deflections of the vertical from gravity anomalies
Online Contents | 1952
|Deflections of the vertical from gravity anomalies
Online Contents | 1947
|Tables for the computation of deflections of the vertical from gravity anomalies
Online Contents | 1947
|