Fig. 8From: The role of glacial isostatic adjustment in the present-day crustal motion and sea levels of East AsiaPresent-day height rates from leveling (Zhang et al., 1989) in the two sections of AA′ and BB′ shown in Fig. 3 and Fig. 7. The solid and dashed lines are the results before and after the GIA corrections based on GIA model RF3L20(β=0.4)+ICE-4G. The numbers and error bars indicate the GIA effects and their estimated uncertainties.Back to article page