First GOCE gravity field models derived by three different approaches

By Roland Pail, Sean Bruinsma, F. Migliaccio, C. Förste, H. Goiginger, Wolf-Dieter Schuh, E. Höck, Mirko Reguzzoni, J. Brockmann, O. Abrikosov and 6 more. 2011

544 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Molecular Biology, Oceanography

View Paper: https://www.semanticscholar.org/paper/73f11bccc44f29eea4ea7a4ba03170829eaf9ebd

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Citations in the corpus

GOCO06s – a satellite-only global gravity field model (2020, background): “…are mainly determined by GRACE (up to degree 130), and GOCE is the main contributor to the medium to short wavelengths (degree 130 to 300) (e.g. Pail et al., 2011; Maier et al., 2012; Yi et al., 2013 Primary focus of combined models is the static gravity ﬁeld (e.g. Pail et al., 2010; Farahani…”
GOCE gravitational gradiometry (2011, methodology): “The accuracy of the spherical harmonic coefficients determined from the measured gradients, and to a small extent also spatial resolution, will increase with increasing the number of measurement cycles (see Pail et al. 2011).”
Geophysics From Terrestrial Time‐Variable Gravity Measurements (2017, background): “For completeness let us mention other satellites such as the Laser Geodynamic Satellite (LAGEOS) (Seeber, 2003), the Challenging Minisatellite Payload (CHAMP) (Reigber et al., 2002), and the Gravity field and steady-state Ocean Circulation Explorer (GOCE) (Pail et al., 2011).”
GECO: a global gravity model by locally combining GOCE data and EGM2008 (2016, unknown): “In this last case the ESA official global gravity models are derived by applying three different approaches (Pail et al., 2011) and among them the fifth release of the time-wise GOCE solution (here called GOCE-TIM-R5) going till degree 280 can be cited (Brockmann et al., 2014).”
Gravity and Topography of the Terrestrial Planets (2015, background): “…in 2009; Floberghagen et al., 2011; Rummel et al., 2011) is providing highly accurate estimates of the Earth’s long-wavelength gravity field (corresponding to spherical harmonic degrees less than about 200; Pail et al., 2011) and time variations in gravity resulting from geologic processes.”
Validation of GOCE gravity field models by means of orbit residuals and geoid comparisons (2011, background): “Details of the processing characteristics are summarized in Pail et al. (2011).”