Table 1 Climate conditions and ice sheet contributions to global mean sea level during three past warm periods that are often used as analogues for current or near-future climate conditions: Marine Isotope Stage (MIS) 5e, MIS 11 and the Mid Pliocene Warm Period (MPWP), Published data sources used to compile the Table are available in Supplementary Table 1
Marine Isotope Stage 5e (~129 –116 ka) | Marine Isotope Stage 11 (~400 ka) | Mid-Pliocene Warm Period (3.3–2.9 Ma) | ||
---|---|---|---|---|
Forcing (peak values) | CO2 | 287 ppm | 286 ppm | 350–450 ppm |
Global mean temp. anomalyb | 1 °C | 1–2? °C | 2–5 °C | |
'Arctic’ temp. anomalyc | 4–8 °C | 4–10 °C | 4–11 °C | |
'Antarctic’ temp. anomalyc | 4–5 °C | 2–3 °C | ? °C | |
Greenland | Ice sheet response | Central portion of ice sheet largely intact; southern GrIS deglaciated | NW and southern GrIS deglaciated; complete deglaciation possible | Partial to complete deglaciation |
GMSL contribution | Estimates range from 1 to >5 m | Estimates include: >1.4 m, 4.5–6 m; 6.1 (3.9–7) m | Up to 7.4 m | |
Antarctica | Ice sheet response | WAIS retreat, some EAIS retreat possible | EAIS retreat & increased runoff indicated | Retreat in WAIS and EAIS |
GMSL contribution | Debated, up to 5 m (or higher if EAIS contributed) | Uncertain; up to 3–4 m | Possibly 13–17 m | |
Peak GMSL | 2–9 m above present | 6–13 m above present | 10–20 m above present | |
Interpretationa | GMSL exceeded present (H); A portion of the GrIS retreated (H); AIS contributed to GMSL rise (M) | GMSL exceeded present (M-H); GrIS smaller than present (H); majority of the GrIS melted (M-H); AIS smaller than present (M) | GrIS smaller than present (H); AIS smaller than present (H) |