Coupling of ice‐shelf melting and buttressing is a key process in ice‐sheets dynamics

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The stability of grounding lines on retrograde slopes (2012, methodology): “Elmer/Ice and Úa, have been used extensively in the past to calculate grounding-line migrations for various different setups (Durand et al., 2009a; Gagliardini et al., 2010; Pattyn et al., 2012).”
Continental scale, high order, high spatial resolution, ice sheet modeling using the Ice Sheet System Model (ISSM) (2012, background): “…2012 F01022 1 of 20 and ice shelf areas, but their assumptions are not strictly valid near grounding lines where a full-Stokes model (FS) is significantly more accurate [Lestringant, 1994; Nowicki and Wingham, 2008; Durand et al., 2009a, 2009b; Gagliardini et al., 2010; Morlighem et al., 2010].”
A three-dimensional full Stokes model of the grounding line dynamics: effect of a pinning point beneath the ice shelf (2011, background): “D byLestringant (1994), and more recently by Nowicki and Wingham (2008), Durand et al. (2009a) and Gagliardini et al. (2010).”