Fig. 2: Seasonality of warming in the CMIP5 and CMIP6 extreme high-emission scenarios.
From: Greater Greenland Ice Sheet contribution to global sea level rise in CMIP6
a CMIP5 2 m temperature anomaly (RCP8.5, n = 28) from south to north for the period 2071–2100, compared to the baseline climate of 1961–1990. Different lines represent the warming in four different seasons. b Same as a but for the CMIP6 SSP585 scenario (n = 28). c Difference in warming in 2071–2100 between CMIP6 (SSP585) and CMIP5 (RCP8.5) (positive = more warming in CMIP6).
