1.67 km (1.0 mi) (average), ~3.5 km (2.2 mi) (maximum)[2]
The Greenland ice sheet is an ice sheet which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick, and over 3 km (1.9 mi) thick at its maximum.[2] It is almost 2,900 kilometres (1,800 mi) long in a north–south direction, with a maximum width of 1,100 kilometres (680 mi) at a latitude of 77°N, near its northern edge.[1] The ice sheet covers 1,710,000 square kilometres (660,000 sq mi), around 80% of the surface of Greenland, or about 12% of the area of the Antarctic ice sheet.[2] The term 'Greenland ice sheet' is often shortened to GIS or GrIS in scientific literature.[3][4][5][6]
Greenland has had major glaciers and ice caps for at least 18 million years,[7] but a single ice sheet first covered most of the island some 2.6 million years ago.[8] Since then, it has both grown[9][10] and contracted significantly.[11][12][13] The oldest known ice on Greenland is about 1 million years old.[14] Due to anthropogenic greenhouse gas emissions, the ice sheet is now the warmest it has been in the past 1000 years,[15] and is losing ice at the fastest rate in at least the past 12,000 years.[16]
Every summer, parts of the surface melt and ice cliffs calve into the sea. Normally the ice sheet would be replenished by winter snowfall,[4] but due to global warming the ice sheet is melting two to five times faster than before 1850,[17] and snowfall has not kept up since 1996.[18] If the Paris Agreement goal of staying below 2 °C (3.6 °F) is achieved, melting of Greenland ice alone would still add around 6 cm (2+1⁄2 in) to global sea level rise by the end of the century. If there are no reductions in emissions, melting would add around 13 cm (5 in) by 2100,[19]: 1302 with a worst-case of about 33 cm (13 in).[20] For comparison, melting has so far contributed 1.4 cm (1⁄2 in) since 1972,[21] while sea level rise from all sources was 15–25 cm (6–10 in) between 1901 and 2018.[22]: 5
If all 2,900,000 cubic kilometres (696,000 cu mi) of the ice sheet were to melt, it would increase global sea levels by ~7.4 m (24 ft).[2] Global warming between 1.7 °C (3.1 °F) and 2.3 °C (4.1 °F) would likely make this melting inevitable.[6] However, 1.5 °C (2.7 °F) would still cause ice loss equivalent to 1.4 m (4+1⁄2 ft) of sea level rise,[23] and more ice will be lost if the temperatures exceed that level before declining.[6] If global temperatures continue to rise, the ice sheet will likely disappear within 10,000 years.[24][25] At very high warming, its future lifetime goes down to around 1,000 years.[20]
^Thiede, Jörn; Jessen, Catherine; Knutz, Paul; Kuijpers, Antoon; Mikkelsen, Naja; Nørgaard-Pedersen, Niels; Spielhagen, Robert F (2011). "Millions of Years of Greenland Ice Sheet History Recorded in Ocean Sediments". Polarforschung. 80 (3): 141–159. hdl:10013/epic.38391.
^Reyes, Alberto V.; Carlson, Anders E.; Beard, Brian L.; Hatfield, Robert G.; Stoner, Joseph S.; Winsor, Kelsey; Welke, Bethany; Ullman, David J. (25 June 2014). "South Greenland ice-sheet collapse during Marine Isotope Stage 11". Nature. 510 (7506): 525–528. Bibcode:2014Natur.510..525R. doi:10.1038/nature13456. PMID24965655. S2CID4468457.
^Cite error: The named reference Hörhold2023 was invoked but never defined (see the help page).
^Cite error: The named reference Briner2020 was invoked but never defined (see the help page).
^Cite error: The named reference SROCC3.2ES was invoked but never defined (see the help page).
^Cite error: The named reference CB2022 was invoked but never defined (see the help page).
^Fox-Kemper, B.; Hewitt, H.T.; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S.S.; Edwards, T.L.; Golledge, N.R.; Hemer, M.; Kopp, R.E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S.L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.). "Chapter 9: Ocean, Cryosphere and Sea Level Change"(PDF). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK and New York, NY, US. Archived(PDF) from the original on 24 October 2022. Retrieved 22 October 2022.
^ abCite error: The named reference Aschwanden2019 was invoked but never defined (see the help page).
^Cite error: The named reference Mouginot2019 was invoked but never defined (see the help page).