The evolution of Greenland’s climate and ice volume during 1850–2100.

• 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.g006

(A): Black line: concentration of CO 2 forcing in our climate model simulation. Blue line: yearly mean ocean temperature forcing. Red line: Greenland-wide summer temperature anomalies in respect to the Pre-Industrial values (100 years of climatology mean). (B): Anomaly of ice volume of the GrIS with respect to the Pre-Industrial values. The solid lines are the simulations using initial conditions obtained by the paleo-spinup, while the dashed lines are the results using initial conditions obtained by a ten thousand year Pre-Industrial equilibrium-spinup. The coloured lines are the results from individual ensemble members (see Table 1 ), and the thick black lines are the results of the ensemble mean.