Modelling post-glacial rebound with lateral viscosity variations

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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): “The dynamic ocean load is implemented through the self-gravity iteration (see also Wu 2004; Paulson et al. 2005).”
Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions (2018, methodology): “However, an increasing number of studies are making use of a framework that can accommodate three-dimensional variations in mantle viscosity (e.g. Ivins and Sammis, 1995; Martinec, 2000; Latychev et al., 2005b; Kaufmann et al., 2005; Paulson et al., 2005; Steffen et al., 2006; A et al., 2013), possi”