Note extreme temperature maximums of 5 - 8 °C and that multiple ice, atmosphere and ocean processes help
reinforce albedo feedbacks (after Wood et al., submitted).
Not exact matches
It's the same series of an initial forcing (change in insolation due to Milankovitch orbital cycles) being amplified by
reinforcing feedbacks (change in
albedo, change in temperature and partial pressure regulating both CO2 and H2O), but in reverse from an exit from a glacial period.
However, the contributions of water vapour / lapse rate and surface
albedo feedbacks to sensitivity spread are non-negligible, particularly since their impact is
reinforced by the mean model cloud
feedback being positive and quite strong.