(A, left) Ice thickness and (B, right) surface ice velocity anomaly between the initial conditions obtained from the equilibrium-spinup and paleo-spinup (equilibrium minus paleo).

• 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.g008

Black line represents the coastline. As shown, individual glaciers have distinct responses. Overall, northeastern Greenland contributes to a larger GrIS ice volume in comparison with the that obtained from the paleo-spinup. With respect to the surface ice velocity, large portions of the GrIS show faster ice velocity in the equilibrium-spinup with respect to that obtained from paleo-spinup. Results are the ensemble mean of the seven ensemble members.