Fig. 6From: The role of glacial isostatic adjustment in the present-day crustal motion and sea levels of East AsiaEffects of ice model. Left panels show present-day uplift rates (a), tangential rates (c), and geoid rates (e) in East Asia predicted by model RF3L20(β=0.4)+ICE-5G. Right panels show their difference when compared with model RF3L20(β=0.4)+ICE-4G (Fig. 3(a, b, c)). Units are in mm/yr.Back to article page