Fig. 7: The viscous relative sea-level (RSL) signal from projected ice-sheet change.
From: Projections of 21st-century sea-level fall along coastal Greenland
The elastic contribution (a) versus viscous contribution (b) to total RSL change (c) caused by projected ice-sheet changes under RCP 2.6 at 2100 CE relative to 2017 CE. The percent of the total caused by the viscous response is shown in (d).
