WRT our current discussion of ice sheet dynamics, the latest IPCC report actually has * less * to offer in terms of
icesheet change predictions precisely because there have been so many new findings and such dramatic changes in just the last few years.
Not exact matches
Perhaps you might want to read that paper as well as «Climate
Change and Trace Gases», available in many places, which argues for an albedo flip mechanism and (relatively) short timescales for
icesheet response to forcing, based on paleo data.
That makes it somewhat easier to estimate
changes in Greenland and Antarctic
icesheets, but very much remains unknown even in this forced case.
Radiative perturbation from
icesheet and
changed sealevel is estimated -3.2 W / m2 (with higher uncertainties than GHG), Vegatation and aerosols estimated -1 W / m2.
These
changes resulted in more sunlight on the N. hemisphere where the most extensive
icesheets were.