Extended Data Fig. 4: Sensitivity experiment showing the influence of basal friction on simulated GIS mass change.
From: Rate of mass loss from the Greenland Ice Sheet will exceed Holocene values this century
The simulated ice-mass change (Gt per century) in the Holocene is shown using climatologies from model run 1 (Extended Data Table 1), with reference friction coefficients outside the present-day ice margin derived as a function of the bed topography (red) or as an extrapolation of friction coefficients (blue).
