An Earth gravity field model complete to degree and order 150 from GRACE: EIGEN-GRACE02S

By C. Reigber, R. Schmidt, Frank Flechtner, Rolf König, U. Meyer, K. Neumayer, P. Schwintzer, S. Zhu. 2005

359 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Molecular Biology, Oceanography

View Paper: https://www.semanticscholar.org/paper/0bf76ede50a611420b6f7489495bb4b0d44d78ea

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Citations in the corpus

The GeoForschungsZentrum Potsdam/Groupe de Recherche de Gèodésie Spatiale satellite-only and combined gravity field models: EIGEN-GL04S1 and EIGEN-GL04C (2008, methodology): “…while the published EIGENGRACE02S, EIGEN-GRACE03S and EIGEN-GL04S1 solutions had been computed using a stabilization of the underlying normal equations by stochastic a priori information for the short wavelength spherical harmonic coefficients beyond a certain degree (e.g. Reigber et al. 2005).”
GECO: a global gravity model by locally combining GOCE data and EGM2008 (2016, neutral): “In the last decades different methods have been developed to produce global gravity models (see, among others, Lerch et al., 1972; Rapp, 1975, 1984; Balmino et al., 1976; Wenzel, 1985; Lemoine et al., 1998; Tscherning, 2001; Reigber et al., 2005; Pavlis et al., Stud.”
Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques (2009, methodology): “The first guess is a large-scale MDT field based on the EIGEN02S geoid model (Reigber et al. 2005) and the Collecte Localisation Satellites 2001 (CLS01) mean sea surface (Hernandez et al.”
Bias-corrected regularized solution to inverse ill-posed models (2012, background): “Regularization has also been widely applied to solve inverse ill-posed geodetic problems, in particular, those in satellite gravimetry (see, e.g., Schaffrin 1980; Xu 1992, 1998; Xu and Rummel 1994a; Reigber et al. 2005).”
Phenomenology of the Lense-Thirring effect in the solar system (2010, methodology): “GRACE recovers the spherical harmonic coefficients of the geopotential from the tracking of both satellites by GPS and from the observed intersatellite distance variations (Reigber et al. 2005).”
Variations of the Earth's figure axis from satellite laser ranging and GRACE (2011, background): “satellite‐only mean gravity fields [Tapley et al., 2004, 2005, 2007; Reigber et al., 2005; Forste et al., 2008].”
What Can be Expected from the GRACE-FO Laser Ranging Interferometer for Earth Science Applications? (2016, neutral): “The high–low SST GPS phase and code observations, used to define a reference frame for LEO orbit integration (Reigber et al. 2005) have been simulated with white noise of 0.”