ESA's satellite-only gravity field model via the direct approach based on all GOCE data

• Published in: Geophysical research letters Vol. 41; no. 21; pp. 7508 - 7514
• Main Authors: Bruinsma, Sean L., Förste, Christoph, Abrikosov, Oleg, Lemoine, Jean-Michel, Marty, Jean-Charles, Mulet, Sandrine, Rio, Marie-Helene, Bonvalot, Sylvain
• Format: Journal Article
• Language: English
• Published: Washington Blackwell Publishing Ltd 16.11.2014; John Wiley & Sons, Inc
• Subjects: Altitude; Calibration; Circulation; Climate; Construction; Data; Data processing; Data recovery; Earth; Earth gravitation; geodesy and gravity; Geoid; Geoids; GOCE (experiment); GRACE (experiment); Gravitation; Gravitational fields; Gravity; Gravity field; LAGEOS (satellite); Marine; Ocean circulation; Ocean currents; Ocean models; Optimization; Recovery; Resolution; Satellites; Steady state; Water circulation
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1002/2014GL062045

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. Key Points Model based on LAGEOS, GRACE, and all GOCE dataCalibrated geoid error at 100 km resolution of 1.7 cmImproved geostrophic ocean circulation on 100–200 km scales