The simulated evolution of the (A, top) ice volume, (B, center) ice temperature (average over entire GrIS) and (C, bottom) dynamic ice loss in the paleo-spinup (solid lines) and the equilibrium-spinup (dashed lines).

• Main Authors: Hu Yang (521488), Uta Krebs-Kanzow (11979695), Thomas Kleiner (11979698), Dmitry Sidorenko (5260150), Christian Bernd Rodehacke (11979701), Xiaoxu Shi (8560299), Paul Gierz (11979704), Lu Niu (2589736), Evan J. Gowan (4884178), Sebastian Hinck (11979707), Xingxing Liu (715957), Lennert B. Stap (11979710), Gerrit Lohmann (7018322)
• Format: Still Image
• Language: unknown
• Published: 2022
• Subjects: Evolutionary Biology; Ecology; Environmental Sciences not elsewhere classified; Biological Sciences not elsewhere classified; several thousand years; 6 &# 8211; minimum ice volume; greenland &# 8217; 5 ka lag; greenland ice sheet; recent climate changes; late 20th century; gris experienced growth; ice volume response; holocene climate needs; ice sheet simulations; holocene thermal maximum; especially holocene climate; ice volume; 20th century; slow response; recent timing; entire holocene; 17 ka; 125 ka; simulation implies; second half; results highlight; respective extremes; pism ); last interglacial; industrial era; getting colder; esm ); equilibrium throughout; begin earlier; background trend; 2100 ad; Greenland; Ice Sheet
• Online Access: https://doi.org/10.1371/journal.pone.0259816.g007

All results are given as anomalies with respect to the corresponding Pre-Industrial (i.e., 1850) values. The coloured lines are results from individual ensemble members, and the thick black lines are the ensemble mean.