Large scale ocean circulation from the GRACE GGM01 Geoid

By Byron D. Tapley, D. Chambers, Srinivas V. Bettadpur, John C. Ries. 2003

158 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Molecular Biology, Oceanography

View Paper: https://www.semanticscholar.org/paper/77b97db76136cf5b487254f10b1f9ef5e100f14f

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In Earth-Surface Processes

B. Galperin

In Molecular Biology

In Oceanography

Citations in the corpus

Intersatellite laser ranging instrument for the GRACE follow-on mission (2012, methodology): “The Gravity Recovery and Climate Experiment (GRACE) has successfully demonstrated the use of intersatellite ranging between two satellites in low-Earth orbit for monitoring of the spatial and time variable of Earth's gravity field (Tapley et al. 2003, 2004b).”
Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques (2009, methodology): “In method A, we use hA computed as the difference of the Goddard Space Flight Center Mean Sea Surface 2000 (GSFCMSS00) time-mean sea surface and GRACE Gravity Model 2002 (GGM02C) geoid models (available online at http://grace.jpl.nasa.gov/data/dot/; Tapley et al. 2003; Fig.”
Assimilating Along-Track Altimetric Observations through Local Hydrostatic Adjustment in a Global Ocean Variational Assimilation System (2011, methodology): “MDTs based solely on space-borne gravimetric observations (Tapley et al. 2003) and adjusted by means of in situ observations (Rio and Hernandez 2004, hereafter RIO04) may not represent the mean dynamic topography seen by the ocean model (Vidard et al. 2009).”
An Earth gravity field model complete to degree and order 150 from GRACE: EIGEN-GRACE02S (2005, methodology): “The striking gain in accuracy and resolution with respect to pre-CHAMP and the CHAMP-only models is obvious, also the benefit of improved processing in the EIGEN-GRACE02S solution with respect to the early GRACE solutions GGM01S and EIGEN-GRACE01S.”
GGM02 – An improved Earth gravity field model from GRACE (2005, methodology): “The resulting topography maps are smoothed as before (Tapley et al. 2003, Eq.”
The gravity recovery and climate experiment: Mission overview and early results (2004, background): “It has been shown that these changes represent improvements, particularly in the equatorial region, the Antarctic circumpolar region and in the regions occupied by western boundary currents [Tapley et al., 2003].”
The GeoForschungsZentrum Potsdam/Groupe de Recherche de Gèodésie Spatiale satellite-only and combined gravity field models: EIGEN-GL04S1 and EIGEN-GL04C (2008, background): “A description of the test algorithm can be found in Tapley et al. (2003).”