Fig. 5: Scaling of SMB model runoff estimates.
From: Vertical bedrock shifts reveal summer water storage in Greenland ice sheet

Scaling factors for warm (a), ordinary (b) and cold (c) years, to be applied to the SMB model runoff estimates to achieve a best match with GNET station observed vertical displacements. Error bars are defined on the basis of the 1st and the 3rd quartiles as the lower and upper bounds, respectively, from 100 Monte Carlo runs.