Fig. 5.

Break-down of projected ESL contributions and of their uncertainty. Projected increase of the 100-year ESL from changes in climate extremes, the high tide water level, as well as from SLR contributions from Antarctica, land-water, Greenland, glaciers, dynamic sea level (DSL), glacial isostatic adjustment (GIA), and steric-effects (a, b); variance (in m²) in components (c, d) and fraction of components’ variance in global ESL change (e, f); under RCP4.5 (a, c, e) and RCP8.5 (b, d, f). Colors represent different components as in the legend and values express the global mean of the median