GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE
By W. Richard Peltier. 2004
2,799 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Chemistry, Oceanography
View Paper: https://www.semanticscholar.org/paper/3e88fbfee7844394bc96f62b36bed5a0396ba669
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In Atmospheric Science
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- John M. Wahr
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- Isabella Velicogna
- Ernst J. O. Schrama
- F. Landerer
- W. Wal
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In Environmental Chemistry
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- John M. Wahr
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In Oceanography
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Citations in the corpus
- Antarctic mass rates from GRACE (2006, neutral): “Published models of PGR, from estimated ice load histories and assumed lithosphere and mantle properties are available for the entire globe [e.g., Peltier, 2004 ] and for the Antarctic continent [Ivins and James, 2005].”
- Greenland mass balance from GRACE (2005, methodology): “To isolate the present-day ice mass signal we independently estimate the PG secular gravity signal and remove it from the GRACE trend given in Section 4. We use the ICE-5G global ice history model of Peltier [2004] , convolved with viscoelastic Green’s functions for an incompressible Earth, compute”
- Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation (2009, methodology): “The ice-sheets are imposed and based on the reconstruction from Peltier (2004) ICE-5G.”
- Phylogenetic endemism in terrestrial mammals (2015, background): “LGM climate includes temperature (MAT LGM), precipitation (PREC LGM) (Braconnot et al., 2007) and LGM glacial extent (Peltier, 2004).”
- The land ice contribution to sea level during the satellite era (2017, methodology): “It implies a positive contribution from land hydrology and/or other factors such as a GIA trend on ocean basin volume closer to the lower end of estimates of −0.15 mm yr−1 (Tamisiea 2011).”
- Probabilistic assessment of sea level during the last interglacial stage (2009, neutral): “[15] Mitrovica, J.”
- Improved methods for observing Earth's time variable mass distribution with GRACE using spherical cap mascons (2015, methodology): “All data have been processed such that the C20 coefficients have been replaced with an SLR-derived value [Cheng and Tapley, 2004], degree 1 terms have been calculated according to Swenson et al. [2008], and glacial isostatic adjustment (GIA) signals have been removed using the Paulson model [Paulson”
- Optimizing estimates of annual variations and trends in geocenter motion and J2 from a combination of GRACE data and geophysical models (2016, methodology): “, 2012] is based on the ICE-5G ice history and a simplified version of mantle viscosity model VM2 [Peltier, 2004] and computed for a compressible Earth model.”
- Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica (2015, methodology): “The maximum uplift rate for model HF10D in Antarctica is larger than the VM2 uplift rate there, while in North America and Scandinavia the HF10D uplift rates are below the VM2 uplift rates (see van der Wal et al., 2013, Fig.”
- Antarctica, Greenland and Gulf of Alaska land-ice evolution from an iterated GRACE global mascon solution (2013, methodology): “For both the GIS and GOA, a GIA model based on the ICE-5G deglaciation history and an incompressible two-layer approximation to the VM2 viscosity profile are used to correct the GRACE mascon solution (Paulson and others, 2007, computed and provided by A. Geruo, 2011).”