Simulations of Antarctic Ice Sheet sensitivity to climate and ocean forcing for a suite of Antarctic palaeotopographies

The ice sheet model output reflect quasi-equilibrium conditions and are gridded at 10 km horizontal resolution. The ice sheet model includes parameterisations for the marine ice cliff failure and marine ice shelf hydrofracture processes. Full asynchronous coupling feedback between the regional climate model and the ice sheet model is not performed; the ice sheet extent in the regional climate model was kept constant.