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By 2100, net ice loss from Antarctica alone would add around 11 cm (5 in) to the global sea level rise. Further, the way WAIS is located deep below the sea level leaves it vulnerable to marine ice sheet instability, which is difficult to simulate in ice sheet models. If instability is triggered before 2100, it has the potential to increase ...
At the beginning and ending points, and approximately every 50 to 75 km in between, a station was set up for the following work: a vertical 40-m hole was bored into the ice, the density and temperature of the ice at various depths in the borehole were measured, the ice sheet was sounded seismically, the accumulation rate was studied in hand ...
Earth's North Pole is covered by floating pack ice over the Arctic Ocean. Portions of the ice that do not melt seasonally can get very thick, up to 3–4 meters thick over large areas, with ridges up to 20 meters thick. One-year ice is usually about 1 meter thick. The area covered by sea ice ranges between 9 and 12 million km 2.
The ice sheet is around 2.2 km (1.4 mi) thick on average and is 4,897 m (16,066 ft) at its thickest point. [78] It is also home to the geographic South Pole, South Magnetic Pole and the Amundsen–Scott South Pole Station. The surface of the EAIS is the driest, windiest, and coldest place on Earth.
If ice shelves break up, the ice flow behind them may accelerate, resulting in increasing melt of the Antarctic ice sheet and an increasing contribution to sea level rise. Known changes in coastline ice around the Antarctic Peninsula: 1936–1989: Wordie Ice Shelf significantly reduced in size. 1995: Ice in the Prince Gustav Channel disintegrated.
The loss of this ice sheet would take between 2,000 and 13,000 years, [39] [40] although several centuries of high greenhouse emissions could shorten this time to 500 years. [41] A sea-level rise of 3.3 m (10 ft 10 in) would occur if the ice sheet collapses, leaving ice caps on the mountains, and 4.3 m (14 ft 1 in) if those ice caps also melt. [42]
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