Fig. 7From: The role of glacial isostatic adjustment in the present-day crustal motion and sea levels of East AsiaUncertainties in the present-day GIA observables (in Fig. 3) predicted by model RF3L20(β=0.4)+ICE-4G. (a) uplift-rate uncertainties; (b) tangential-rate uncertainties; (c) geoid-rate uncertainties. The units for the scale bars on the right are in mm/yr. Black circles with numbers denote the geodetic stations listed in Table 1.Back to article page