GGM02 – An improved Earth gravity field model from GRACE
By Byron D. Tapley, John C. Ries, Srinivas V. Bettadpur, D. Chambers, M. Cheng, F. Condi, Brian C. Gunter, Z. Kang, P. Nagel, R. Pastor and 3 more. 2005
674 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Molecular Biology, Oceanography
View Paper: https://www.semanticscholar.org/paper/aff2803dcb323349b7d4732c3f54a465b69b5841
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Astronomy and Astrophysics
- Sean Bruinsma
- H. Lichtenegger
- R. O’Connell
- Lorenzo Iorio
- Anders Søndberg Sørensen
- Byron D. Tapley
- Christian Corda
- Matteo Luca Ruggiero
In Molecular Biology
- Byron D. Tapley
- Sean Bruinsma
- John C. Ries
- Srinivas V. Bettadpur
- R. Schmidt
- David T. Sandwell
- Walter H. F. Smith
- H. Lichtenegger
In Oceanography
- Byron D. Tapley
- John C. Ries
- Srinivas V. Bettadpur
- Sean Bruinsma
- David T. Sandwell
- Walter H. F. Smith
- R. Schmidt
- Matthew Amos
Citations in the corpus
- The new gravimetric quasigeoid model KTH08 over Sweden (2009, methodology): “GGM error Published ones for GGM02C (Tapley et al. 2005) and EGM 96 (Lemoine et al.”
- Phenomenology of the Lense-Thirring effect in the solar system (2010, background): “18L. I. thanks M Watkins (JPL) for having provided me with the even zonals and their sigmas of the JEM01-RL03B model. from GFZ (Potsdam, Germany), GGM02S (Tapley et al. 2005) and GGM03S (Tapley et al. 2007) from CSR (Austin, Texas), ITG-Grace02s (Mayer-Gürr et al. 2006), ITG-Grace03s (Mayer-Gürr 2”
- The GeoForschungsZentrum Potsdam/Groupe de Recherche de Gèodésie Spatiale satellite-only and combined gravity field models: EIGEN-GL04S1 and EIGEN-GL04C (2008, methodology): “GGM02C (Tapley et al. 2005) is a combination solution complete up to degree and order 200 incorporating GRACE satellite data and EGM96-spherical harmonic coefficients obtained from NGA surface gravity data.”
- Global marine gravity from retracked Geosat and ERS‐1 altimetry: Ridge segmentation versus spreading rate (2009, methodology): “The longer wavelength gravity field is more accurately measured at orbital altitude using spacecraft such as CHAMP [Reigber et al., 2002], GRACE [Tapley et al., 2005], and GOCE [Klees et al., 2000].”
- Source parameter inversion for recent great earthquakes from a decade‐long observation of global gravity fields (2013, methodology): “Next, we formulate inverse models to estimate the moment tensor components and subsequently fault parameters from the GRACE data for each earthquake.”
- Gravity and Topography of the Terrestrial Planets (2015, background): “Finally, the topography and gravitational field of Earth are continually being refined, most notably by a series of recent and ongoing missions such as GRACE (Gravity Recovery and Climate Experiment; Tapley et al., 2005) and GOCE (Gravity Field and Steady-State Ocean Circulation Explorer; Drinkwater”
- Precise orbit determination for the GRACE mission using only GPS data (2006, methodology): “The main differences between our old and new GRACE POD investigations are the gravity models (GGM01C versus GGM02C), ocean tide models (CSR 4.0 versus FES2004), arc lengths (30 vs 24 h) and test data sets (5 days vs 4 months).”
- A quantum network of clocks (2013, background): “Besides creating a world platform for time and frequency metrology, such a network may find important applications to a range of technological advances for earth science [41] and to the test and search for the fundamental laws of nature, including relativity and the connection between quantum and gr”
- Unification of New Zealand’s local vertical datums: iterative gravimetric quasigeoid computations (2009, methodology): “The above data were used, together with a “cut and paste” combination of GGM02S (Tapley et al. 2005) and EGM96 (Lemoine et al.”
- Geodynamics of the Yellowstone hotspot and mantle plume: Seismic and GPS imaging, kinematics, and mantle flow (2009, background): “The significance of some important hotspots are also seen in the Earth's gravity field (Tapley et al., 2005), where notable longwavelength positive anomalies, in excess of 800 km, are associated with the Hawaii, Iceland, and Yellowstone hotspots (Fig.”