The evolution of Greenland’s climate and simulated ice volume of the GrIS from the last interglacial to the Pre-Industrial era.

• 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.g004

(A): The prescribed forcing of summer (JJA) atmospheric temperature (red line), yearly mean ocean temperature (blue line) and global mean sea level (black line). (B): The simulated ice volume evolution of the GrIS. The coloured lines are the results from individual ensemble members (see Table 1 ). The thick black line gives the ensemble mean values. The red shadow area marks the time period when Greenland’s climate gets warmer, and the blue patch illustrates the time when Greenland’s climate colds.