Gravity anomalies from satellite altimetry: comparison between computation via geoid heights and via deflections of the vertical

Bulletin Géodésique

Volumn 69, Issue 4, 1995, Pages 252-260

  Olgiati, A ^a   Balmino, G ^a   Sarrailh, M ^a   Green, C M ^b  

^a CNES   (France)

^b UNIVERSITY OF LEEDS   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0009612119     PISSN: 00074632     EISSN: 14321394     Source Type: Journal    
DOI: 10.1007/BF00806737     Document Type: Article

References (19)

1. A new method of interpolation and smooth curve fitting based on local procedures
2. The geodetic approximations in the conversion of geoid height to gravity anomaly by Fourier transform
3. Geoid computations by the multi-band spherical FFT approach
4. Digital images of combined oceanic and continental data sets and their use in tectonic studies
5. Altimetric gravity anomalies in the Norwegian-Greenland Sea — Preliminary results from the ERS-1 35 days repeat mission
6. Comparison of marine gravity from shipboard and highdensity satellite altimetry along the Mid-Atlantic Ridge
7. Oceanwide gravity anomalies from Geos-3, Seasat and Geosat altimeter data
8. Biharmonic spline interpolation of Geos-3 and Seasat altimeter data
9. Antartic marine gravity field from high-density satellite altimetry
10. The use of FFT techniques in physical geodesy
11. Gridding with continuous curvature splines in tension
12. Stokes formula using Fast Fourier Techniques
13. The determination of a one year mean sea surface height track from Geosat altimeter data and ocean variability implications