Extended Data Fig. 4: Comparison between the rate of relative sea-level change simulated by 1D and 3D Earth models.
From: Sea-level rise at the end of the last deglaciation dominated by North American ice sheets
a, Mississippi Delta, b, Yangtze Delta, c, Rhine-Meuse Delta, d, Malay Peninsula. The solid lines show rates generated from the 1D Earth models used in the present study (Extended Data Table 1); the dashed lines show rates generated from six 3D Earth models, with two different global lithosphere models (‘AF’ for the model of Afonso et al. (2018) and ‘YO’ for the model of Yousefi et al. (2021)) and three different seismic models to infer lateral viscosity variations: ‘S40’, ‘SAV’, ‘SEM’(for, respectively, S40RTS, Savani, and SEMUCB-WM1; see Methods for more information).
