Dynamical processes involved in the retreat of marine ice sheets

By R. Hindmarsh, Emmanuel Le Meur. Journal of Glaciology, 2001

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Marine ice-sheet dynamics. Part 1. The case of rapid sliding (2007, background): “Näıvely, one might expect a sensible boundary-layer structure to arise when the ice thickness at the grounding line is comparable with the ice thickness inland in the grounded sheet, and this is in fact implicit in some numerical studies of marine icesheet dynamics (e.g. Hindmarsh & LeMeur 2001).”
Marine ice-sheet profiles and stability under Coulomb basal conditions (2015, background): “Interest in ice sheet stability has also prompted a number of theoretical investigations on the topic, starting with Weertman (1974) and more recently with Hindmarsh and LeMeur (2001), Wilchinsky (2001), and Schoof (2007b).”
Assessing the ability of numerical ice sheet models to simulate grounding line migration (2005, background): “However, the inclusion of internal oscillations, either specified or generated via the MacAyeal-Payne thermal mechanism, does produce the observed range of grounding line migration [Hindmarsh and LeMeur, 2001].”