Antarctic contribution to sea level rise observed by GRACE with improved GIA correction
By Erik Ivins, T. James, John M. Wahr, Ernst J. O. Schrama, F. Landerer, K. Simon. 2013
256 citations recorded by the source corpus.
Subfields: Atmospheric Science, Molecular Biology, Oceanography
View Paper: https://www.semanticscholar.org/paper/e4c80dc3faf98b0b88e52b8c19e70dcb1f0b850c
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
- Isabella Velicogna
- John M. Wahr
- F. Landerer
- David Wiese
- Bryant D Loomis
- Ernst J. O. Schrama
- Scott B. Luthcke
In Molecular Biology
- Isabella Velicogna
- P. Whitehouse
- John M. Wahr
- David Wiese
- F. Landerer
- Bryant D Loomis
- M. Watkins
- Scott B. Luthcke
In Oceanography
- Isabella Velicogna
- F. Landerer
- P. Whitehouse
- John M. Wahr
- David Wiese
- Bryant D Loomis
- Scott B. Luthcke
- M. Watkins
Citations in the corpus
- Improved methods for observing Earth's time variable mass distribution with GRACE using spherical cap mascons (2015, methodology): “This model is again considered to be conservative, particularly for Antarctica where a new generation of models shows the GIA correction to be considerably smaller [Ivins et al., 2013].”
- Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica (2015, methodology): “The three models HF10D, S4D, and S10W will be used to investigate the range in predictions one can get from 3D models.”
- Improved Earth Oblateness Rate Reveals Increased Ice Sheet Losses and Mass‐Driven Sea Level Rise (2019, result): “, 2018) and that our reported values have applied the IJ05_R2 model (Ivins et al., 2013) following several previous studies (Luthcke et al.”
- GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, methodology): “A scaled version of the ANU ice history (Lambeck et al., 2010, 2014) was employed, except for Antarctica and Patagonia where ice models having more contemporary constraints are available (Briggs & Tarasov, 2013; Ivins & James, 2004; Ivins et al., 2013; Whitehouse, Bentley, Milne, et al., 2012).”
- Replacing GRACE/GRACE‐FO C30 With Satellite Laser Ranging: Impacts on Antarctic Ice Sheet Mass Change (2020, methodology): “Ivins et al. (2013) report a 1-σ error of 13 Gt year−1, while Loomis et al.”
- Geophysics From Terrestrial Time‐Variable Gravity Measurements (2017, background): “Hence, investigating the GIA is necessary for studies of past and present ice mass balance (Ivins et al., 2013; Mémin et al., 2011; Omang & Kierulf, 2011).”
- Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions (2018, methodology): “…primary motivation for the recent focus on developing GIA models for Greenland and Antarctica has been to permit accurate interpretation of GRACE data, partitioning the mass change time series into contributions from GIA and 650 contemporary ice mass change (King et al., 2012;Ivins et al., 2013).”
- Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada (2012, methodology): “Shepherd et al. (2012) use two newly developed GIA models, W12a (Whitehouse et al. 2012) and IJ05_R2 (Ivins et al. 2013), to compute GIA corrections for GRACE Antarctic mass loss estimates.”
- Continuity of Ice Sheet Mass Loss in Greenland and Antarctica From the GRACE and GRACE Follow‐On Missions (2020, methodology): “We use the regional IJ05 R2 GIA model (Ivins et al., 2013) over Antarctica and the regional Simpson et al. (2009) GIA model over Greenland.”