A new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea‐level change and present‐day uplift rates
By P. Whitehouse, Michael J. Bentley, G. Milne, Matt A. King, I. Thomas. 2012
294 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/b8b0c52546304964f79406ff9a49b0d8bc43e9a3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- P. Whitehouse
- John M. Wahr
- Ernst J. O. Schrama
- Erik Ivins
- W. Wal
- R. Drummond
- F. Landerer
- W. Richard Peltier
In Oceanography
- P. Whitehouse
- John M. Wahr
- F. Landerer
- Erik Ivins
- Ernst J. O. Schrama
- D. Argus
- W. Richard Peltier
- R. Drummond
Citations in the corpus
- Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model (2015, background): “However, an additional data set has recently become available [Whitehouse et al., 2012a], consisting of exposure age dates on “trimline elevations” PELTIER ET AL.”
- Antarctic contribution to sea level rise observed by GRACE with improved GIA correction (2013, background): “…the AIS volume changes as a function of time since LGM ( 21 ka) for a number of contemporary models including M11 [Mackintosh et al., 2011], W12a [Whitehouse et al., 2012b], and PDcPaSEb [Briggs, 2012], which incorporate local geological constraints, and the ICE-5G (version 1.2) [Peltier, 2004]…”
- Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica (2015, methodology): “Ice model W12a ICE-5G Earth model Whitehouse et al. (2012b) HF10D S4D S10W VM2 Peltier (2004) HF10D S4D S10W Misfit (Eq.”
- The solid Earth’s influence on sea level (2013, background): “…bulge (Mitrovica et al., 2005), both of which may complicate the use of such models to remove the postglacial component from present-day sea-level observations (Chambers et al., 2010; Kendall et al., 2006; King et al., 2012; Métivier et al., 2012; Spada et al., 2012; Whitehouse et al., 2012).”
- Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions (2018, methodology): “…of the lithosphere are often inferred by comparing GIA model output with observations that reflect past and present rates of solid Earth deformation, such as GPS time series or records of past relative 430 sea-level change (e.g. Lambeck et al., 1998;Whitehouse et al., 2012b;Argus et al., 2014).”