Ice sheet
From Wikipedia, the free encyclopedia
An ice sheet is a mass of glacier ice that covers surrounding terrain and is greater than 50,000 km² (19,305 mile²).[1] The only current ice sheets are Antarctic and Greenland; during the last ice age at Last Glacial Maximum (LGM) the Laurentide ice sheet covered much of Canada and North America, the Weichselian ice sheet covered northern Europe and the Patagonian Ice Sheet covered southern South America.
Ice sheets are bigger than ice shelves or glaciers. Masses of ice covering less than 50,000 km² are termed an ice cap. An ice cap will typically feed a series of glaciers around its periphery.
Although the surface is cold, the base of an ice sheet is generally warmer, in places it melts and the melt-water lubricates the ice sheet so that it flows more rapidly. This process produces fast-flowing channels in the ice sheet — these are ice streams.
The present-day polar ice sheets are relatively young in geological terms. The Antarctic Ice Sheet first formed as a small ice cap (maybe several) in the early Oligocene, but retreating and advancing many times until the Pliocene, when it came to occupy almost all of Antarctica. The Greenland ice sheet did not develop at all until the late Pliocene, but apparently developed very rapidly with the first continental glaciation. This had the unusual effect of allowing fossils of plants that once grew on present-day Greenland to be much better preserved than with the slowly forming Antarctic ice sheet.
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[edit] Antarctic ice sheet
The Antarctic ice sheet is the largest single mass of ice on Earth. It covers an area of almost 14 million km² and contains 30 million km³ of ice. Around 90% of the fresh water on the Earth's surface is held in the ice sheet, and, if melted, would cause sea levels to rise by 61.1 metres[2]. In East Antarctica the ice sheet rests on a major land mass, but in West Antarctica the bed is in places more than 2,500 meters below sea level. It would be seabed if the ice sheet were not there. However, if the ice sheet were actually removed, isostatic rebound would occur and Antarctica would rise to an average height of 800 meters above sea level.
[edit] Greenland ice sheet
The Greenland ice sheet occupies about 82% of the surface of Greenland, and if melted would cause sea levels to rise by 7.2 metres[3]. Estimated changes in the mass of Greenland's ice sheet suggest it is melting at a rate of about 239 cubic kilometres (57.3 cubic miles) per year [1]. These measurements came from NASA's Gravity Recovery and Climate Experiment (GRACE) satellite, launched in 2002, as reported by BBC News, 11 August 2006.
[edit] Predicted effects of global warming
Both the Antartic and Greenland ice sheets are predicted to lose mass through melting [4], according to the British Antartic Survey, contradicting early predictions by the IPCC that increased precipitation would occur over the Antarctic[5]. See: sea level rise.
[edit] References
- ^ Glossary of Important Terms in Glacial Geology. Retrieved on 2006-08-22.
- ^ http://www.grida.no/climate/ipcc_tar/wg1/412.htm#tab113
- ^ http://www.grida.no/climate/ipcc_tar/wg1/412.htm#tab113
- ^ http://www.sciencemag.org/cgi/content/full/308/5730/1877
- ^ http://www.grida.no/climate/ipcc_tar/wg1/418.htm
