Extended Data Fig. 3: Relationships between RCP8.5 projections at 2100 and past sea-level changes.
From: Revisiting Antarctic ice loss due to marine ice-cliff instability
a–c, Sea-level contribution at 2100 under RCP8.5 versus sea-level contribution during the Pliocene (a), last interglacial (b) and from 1992 to 2017 (c), for the emulator (small grey dots) and DP16 simulator (large open circles; ref. 6 and R. DeConto, personal communication), with ocean bias correction off (blue) and on (red). Grey shading indicates the DP16 palaeodata range (a, b) or observational mean ± 3 s.d.25 (c); the dashed lines additionally include model error.
