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Assessment of the Greenland ice sheet–atmosphere feedbacks for the next century with a regional atmospheric model coupled to an ice sheet model

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Figure

Figure 1. Evolution of the SMB (black line) and its components from 2005 to 2150 (in m Gt yrand integrated over the ice sheet mask taken from Bamber et al
Figure 3. GrIS surface elevation in 2150 simulated in the 2W ex-periment (in m). The solid black and purple lines represent the equi-librium line altitudes (ELA, limit between the accumulation and theablation zones) in the 2000–2010 and 2090–2100 mean peri
Figure 5. Cumulated SMB (a) and ice flux divergence (b) throughout the entire 2W experiment (from 2000 to 2150) given in metresand computed on the GRISLI grid
Figure 6. (a) Mean surface velocity anomaly (in m yr−1) between the 2140–2150 and the 2000–2010 mean periods for the 2W experiment.(b) Mean surface velocity difference between the NF and the 2W experiments for the 2140–2150 mean period
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