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).

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.

Bibliographic Details
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

Description
Summary:	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.