Fig. 3: Absolute misfit between the SLIP-derived and modelled EuIS RSL signals.
From: Global sea-level rise in the early Holocene revealed from North Sea peats
a–c, The BRITICE-CHRONO14 (a) and ICE6G10 (b,c) reconstructions are here combined with the 1D Earth model that produces the smallest misfit (a,b) and the largest misfit (c) (Extended Data Table 1). For BRITICE-CHRONO, this is a lithosphere thickness of 96 km combined with upper- and lower-mantle viscosities of 0.3 × 1021 Pa s and 20 × 1021 Pa s, respectively. For ICE6G, a lithosphere thickness of 96 km combined with upper- and lower-mantle viscosities of 0.5 × 1021 Pa s and 3 × 1021 Pa s, respectively (very similar to the VM5a Earth model, labelled ICE6G-smallest; b) and a lithosphere thickness of 71 km combined with upper- and lower-mantle viscosities of 0.5 × 1021 Pa s and 5 × 1021 Pa s, respectively (labelled ICE6G-largest; c).
