Hysteresis of the Greenland ice sheet from the Last Glacial Maximum to the future: video of a quasi-equilibrium simulation

Simulating the stability diagram of the Greenland Ice Sheet from an LGM-like state (at -12 K regional summer air temperature anomaly relative to the reference period) to a warming of +4 K with the Yelmo-REMBO coupled model. This is a quasi-equilibrium simulation with a constant forcing rate of 0.00001 K/yr. The right panel shows the evolution of topography and surface velocities, while the left panel shows the volume above flotation as a function of regional summer air temperature anomaly.