Fig. 2
From: Vertical land motion is underestimated in sea-level projections from the Oka estuary, northern Spain
Holocene relative sea-level (RSL) data compared with predictions from 3D glacial isostatic adjustment (GIA) model ICE-6G_C (HetML140). Holocene RSL data showing sea-level index points (SLIP) are plotted as boxes with 2\(\sigma \) vertical and temporal uncertainties and terrestrial and marine limiting data providing upper and lower constraints on RSL, respectively. The RSL comparison plot of 3D GIA model ANU-ICE (HetML140) and RSL data at 13 regions are shown in Fig. S1.
