Fig. 4: Contributions to projected relative sea-level (RSL) change at 2100 CE.
From: Projections of 21st-century sea-level fall along coastal Greenland
Ensemble median and likely range (17th–83rd percentile) of the contributions to RSL change at 2100 CE relative to 2017 CE. RSL change is driven by historical ice changes that occurred during the deglaciation (a, b), the Little Ice Age (c, d) and projected ice-sheet changes under Representative Concentration Pathway (RCP) 2.6 (e, f) or RCP 8.5 (g, h). Other processes, including thermal expansion and ocean dynamics, global glacier change, and land water storage for SSP1-2.6 (i, j) or SSP5-8.5 (k, l), also contribute to RSL change over this century. Projections do not exist within the white areas of panels (i–l).
