Modelling Antarctic and Greenland volume changes during the 20th and 21st centuries forced by GCM time slice integrations

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Will Greenland melting halt the thermohaline circulation? (2006, methodology): “For the 21st century, the projections show a positive contribution of +2 to +7 cm from Greenland that is more than offset by ice sheet growth over Antarctica [Huybrechts et al., 2004].”
Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints (2006, background): “The level of future polar amplification was indeed shown to be dependent on the modern sea–ice thickness and snow cover simulations (Dixon et al. 2003; Holland and Bitz 2003 ).”
Recent Antarctic ice mass loss from radar interferometry and regional climate modelling (2008, background): “Climate warming may increase snowfall in the continent’s interio”
Dangerous human-made interference with climate: a GISS modelE study (2006, unknown): “Huybrechts et al. (2004) use a 3-”
Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries (2006, methodology): “This motivated climate model studies of the future surface mass balance of Antarctica (e.g., Thompson and Pollard 1997; Wild et al. 2003; Huybrechts et al. 2004).”