The model domain of the ice sheet model.

• 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.g001

The model domain of the ice sheet model. The left subpanel shows the ice thickness used to initialise the model (shading) and the contemporary coast line (black contour line) while the right subpanel depicts the corresponding bedrock topography. These data are derived from the ETOPO1 data set [ 42 ].