Fig. 1: Forcing and climate response in CESM2 simulations.
From: The radiative feedback continuum from Snowball Earth to an ice-free hothouse
Time series of (a) specified atmospheric CO2 volume mixing ratio, (b) annual-mean global-mean surface temperature T, and (c) annual-mean global ice area (including sea ice, snow cover on land, and glacial ice), in the Warming simulation (red) and the Cooling simulation (blue). Also included are surface temperature maps averaged over the last decade of the (d) Cooling, (e) pre-industrial (PI) control, and (f) Warming simulations, as well as ice area maps averaged over the last decade of the (g) Cooling, (h) PI control, and (i) Warming simulations (with latitude ϕ and longitude θ). Note that we use the relatively short averaging period of a single decade in these maps in order to better capture the full range given the rates of change near the end of the Warming and Cooling simulations.
