Simultaneous estimation of global present-day water transport and glacial isostatic adjustment

By Xiaoping Wu, M. Heflin, H. Schotman, B. Vermeersen, D. Dong, R. Gross, Erik Ivins, Angelyn W. Moore, S. Owen. 2010

160 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/e319a0d6df59ca30cca2355b8f4fe02ae5465394

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In Atmospheric Science

1. P. Whitehouse
2. Ernst J. O. Schrama
3. W. Wal
4. Makiko Sato
5. Columbia Univ. Earth Institute
6. Centre National de la Recherche Scientifique
7. Karina von Schuckmann Nasa Goddard Institute for Space Studies
8. Jin Li

In Oceanography

1. P. Whitehouse
2. Olivier Francis
3. Olivier de Viron
4. Arnaud Watlet
5. C. Caudron
6. Bruno Meurers
7. Matthew Hecht
8. Columbia Univ. Earth Institute

Citations in the corpus

• Response of the Atlantic Ocean circulation to Greenland Ice Sheet melting in a strongly‐eddying ocean model (2012, background): “It has become increasingly clear that the mass balance of the GrIS is negative [Wu et al., 2010], and that the mass deficit has been increasing [Velicogna, 2009]: from a near-zero balance in the 1970s, estimates of the mass deficit of the GrIS have now reached values close to 300 Gt/yr [Rignot et al”
• Earth's energy imbalance and implications (2011, background): “But at present there is a range of estimates due in part to the difficulty of disentangling ice mass loss from crustal isostatic adjustment (Bromwich and Nicolas, 2010; Sorensen and Forsberg, 2010; Wu et al., 2010).”
• Reducing leakage error in GRACE-observed long-term ice mass change: a case study in West Antarctica (2015, methodology): “Using two published geocenter studies (Wu et al. 2010; Rietbroek et al. 2012) based on joint inversion of GRACE, and GPS, and satellite altimeter data, estimated contributions from long-term geocenter motion to GRACE Antarctic mass rates are ∼32 and ∼13 Gt/year, respectively.”
• Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica (2015, methodology): “…and Wahr, 2006; Chen et al., 2009; King et al., 2012), or (ii) by employing other datasets with different sensitivities to GIA and ice melt such as GPS or satellite altimetry (Wahr et al., 1995, 2000; Riva et al., 2009; Wu et al., 2010; Wang et al., 2013; Sasgen et al., 2013; Gunter et al., 2014).”
• Geophysics From Terrestrial Time‐Variable Gravity Measurements (2017, background): “The glacial isostatic adjustment also modifies geoid at rates up to 1 mm/yr in Greenland, Antarctica, and Fennoscandia (Fleming et al., 2004; Vermeersen & Schotman, 2008; Wu et al., 2010).”
• A new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea‐level change and present‐day uplift rates (2012, methodology): “…uplift from satellite altimetry and GRACE data, and produced an uplift field which has uniformly lower uplift rates compared with IJ05 and ICE-5G. Wu et al. (2010) empirically adjusted the IJ05 model using global geodetic data sets, and produced an estimate of uplift which does not appear to…”
• GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, methodology): “using GRACE is difficult to quantify (see Velicogna & Wahr, 2013), and the full covariance matrix for each of the spherical harmonic coefficients is needed (Wu et al., 2010).”