Marine ice sheet dynamics: Hysteresis and neutral equilibrium

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Coupling of ice‐shelf melting and buttressing is a key process in ice‐sheets dynamics (2010, methodology): “careful way [Schoof, 2007; Durand et al., 2009; Goldberg et al., 2009].”
A three-dimensional full Stokes model of the grounding line dynamics: effect of a pinning point beneath the ice shelf (2011, unknown): “This was also shown by Durand et al. (2009a) using a similar (but 2-”
Continental scale, high order, high spatial resolution, ice sheet modeling using the Ice Sheet System Model (ISSM) (2012, methodology): “…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].”
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). Both models participated in the recently finalised “Marine Ice Sheet Model Intercomparison Project” (MIS”