The influence of continental shelf bathymetry on Antarctic Ice Sheet response to climate forcing

Ice Shelf calving flux (ablation) for seven Parallel Ice Sheet Model simulations using continental shelves of different depths. The thin light-gray lines labeled shallow-, intermediate- and overdeepened-shelf are from Fig. 4 in the manuscript. The wider dashed and solid lines labeled 375 m, 450 m, 525 m and 600 m are the data for other simulations with those approximate average shelf water depths.93