We simulated the Icelandic Ice Sheet over the last 120 kyr using an ice sheet model constrained by geological data with robust uncertainty assessment. At the Last Glacial Maximum, ice reached the continental shelf break, with a potential ice bridge connecting to the Greenland Ice Sheet. Model consistency with geological constraints during deglaciation is only possible with meltwater-driven ice fracture at the ice sheet margin, destabilizing the marine ice sheet and accelerating its collapse.
We simulated the Icelandic Ice Sheet over the last 120 kyr using an ice sheet model constrained...