Closure of the budget of global sea level rise over the GRACE era: the importance and magnitudes of the required corrections for global glacial isostatic adjustment

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Constraining Models of Postglacial Rebound Using Space Geodesy (2008, methodology): “We compare the space geodetic observations against two models of ice sheet thickness as a function of time, ICE-4G (Peltier 1994, 1996, 2002b) and ICE-5G (Peltier 2004, 2007; Peltier & Drummond 2008; Fig.”
Contemporary sea level rise. (2010, methodology): “Post glacial rebound (also called glacial isostatic adjustment, or GIA) is another process that gives rise to vertical land movement.”
Ongoing glacial isostatic contributions to observations of sea level change (2011, methodology): “Our results for the GIA contribution to altimetry observations are in good agreement with predictions from earlier studies (Peltier 2001, 2009) generated using the same Earth and ice sheet models.”
Antarctic contribution to sea level rise observed by GRACE with improved GIA correction (2013, methodology): “[32] Although now clearly in need of revision [e.g., Wang et al., 2013], a ubiquitous GIA model used for correcting GRACE ice mass balance trends has been ICE-5G VM2 [Peltier, 2004, 2009; Riva et al., 2009; Wu et al., 2010].”