Bruinsma S. L., Forste C., Abrikosov O., Lemoine J. M., Marty J. C., Mulet S., Rio M. H., Bonvalot Sylvain. (2014). ESA's satellite-only gravity field model via the direct approach based on all GOCE data. Geophysical Research Letters, 41 (21), p. 7508-7514. ISSN 0094-8276.
Titre du document
ESA's satellite-only gravity field model via the direct approach based on all GOCE data
Bruinsma S. L., Forste C., Abrikosov O., Lemoine J. M., Marty J. C., Mulet S., Rio M. H., Bonvalot Sylvain
Source
Geophysical Research Letters, 2014,
41 (21), p. 7508-7514 ISSN 0094-8276
Gravity field and steady state Ocean Circulation Explorer (GOCE) gravity gradient data of the entire science mission and data from LAGEOS 1/2 and Gravity Recovery and Climate Experiment (GRACE) were combined in the construction of a satellite-only gravity field model to maximum degree 300. When compared to Earth Gravitational Model 2008, it is more accurate at low to medium resolution, thanks to GOCE and GRACE data. When compared to earlier releases of European Space Agency GOCE models, it is more accurate at high degrees owing to the larger amount of data ingested, which was moreover taken at lower altitude. The impact of orbiting at lower altitude in the last year of the mission is large: a model based on data of the last 14 months is significantly more accurate than the release 4 model constructed with the first 28 months. The (calibrated) cumulated geoid error estimate at 100 km resolution is 1.7 cm. The optimal resolution of the GOCE model for oceanographic application is between 100 and 125 km.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020]
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Limnologie physique / Océanographie physique [032]
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Télédétection [126]
