80°S 60°E / 80°S 60°E / -80; 60
41-638: The East Antarctic Ice Sheet ( EAIS ) lies between 45° west and 168° east longitudinally. It was first formed around 34 million years ago, and it is the largest ice sheet on the entire planet, with far greater volume than the Greenland ice sheet or the West Antarctic Ice Sheet (WAIS), from which it is separated by the Transantarctic Mountains . The ice sheet is around 2.2 km (1.4 mi) thick on average and
82-698: A great circle with the 135th meridian east , and it is the reference meridian for the time zone UTC-3 . Starting at the North Pole and heading south to the South Pole , the 45th meridian west passes through: Dome Argus Dome A or Dome Argus is the highest ice dome on the Antarctic Plateau , located 1,200 km (750 mi) inland. It is thought to be the coldest naturally occurring place on Earth , with temperatures believed to reach −90 to −98 °C (−130 to −144 °F). It
123-518: A median of 1.46 m (4 ft 9 in) ( confidence interval between 60 cm (2.0 ft) and 2.89 m (9 ft 6 in)) by 2300, which would involve some loss from the EAIS in addition to the erosion of the WAIS. This Antarctica-only sea level rise would be in addition to ice losses from the Greenland ice sheet and mountain glaciers , as well as the thermal expansion of ocean water. If
164-533: A portion (sometimes overlapping) as their own territory. While relatively small glaciers and ice caps are known to have been present in Antarctica since at least the time of Late Palaeocene , 60 million years ago , a proper ice sheet did not begin to form until the Eocene–Oligocene extinction event about 34 million years ago, when the atmospheric CO 2 levels fell to below 750 parts per million . It
205-413: A third AWS (LGB69) at 70°50′S 77°04′E / 70.833°S 77.067°E / -70.833; 77.067 , 1,854 m (6,083 ft) above sea level, which has operated since January 2002. The station at Dome A is powered by solar cells and diesel fuel and requires yearly service and refuelling. The coldest air temperature recorded by thermometer at Dome A since January 2005
246-502: A whole has low sensitivity to climate change because it is surrounded by the Southern Ocean , which is more effective at absorbing heat than any other ocean due to the currents of the Southern Ocean overturning circulation , very low amounts of water vapor (which conducts heat through the atmosphere) and because of the high albedo (reflectivity) of its icy surface and of the surrounding sea ice . These factors make Antarctica
287-525: Is 4,897 m (16,066 ft) at its thickest point. 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. Lack of moisture in the air, high albedo from the snow as well as the surface's consistently high elevation results in the reported cold temperature records of nearly −100 °C (−148 °F). It
328-687: Is a line of longitude that extends from the North Pole across the Arctic Ocean , Greenland , the Atlantic Ocean , South America , the Southern Ocean , and Antarctica to the South Pole . In Greenland the meridian defines the borders of Avannaata , Qeqertalik , and Qeqqata municipalities with the Sermersooq municipality and the Northeast Greenland National Park . The 45th meridian west forms
369-725: Is a lofty ice prominence, the highest rooftop of the Antarctic Plateau, and the elevation visually is not noticeable. Below this enormous dome, underneath at least 2,400 m (7,900 ft) of ice sheet, lies the Gamburtsev Mountain Range , about the size of the European Alps. The name "Dome Argus" was given by the Scott Polar Research Institute from Greek mythology. Argus built the ship Argo , in which Jason and
410-560: Is about equivalent in size to the European Alps . Consequently, the ice thickness over these mountains ranges from around 1 km (0.62 mi) over their peaks to about 3 km (1.9 mi) over the valleys. These high elevations are an important reason for why the ice sheet is the driest, windiest, and coldest place on Earth. Dome A in particular sets reported cold temperature records of nearly −100 °C (−148 °F). The only ice-free areas of East Antarctica are where there
451-633: Is located 144 km (89 mi) southeast of Dome A, is potentially an even better location to look for the lowest temperatures on Earth. The Polar Research Institute of China deployed a robotic observatory called PLATO (PLATeau Observatory) on the dome in January 2008. PLATO was designed and built by the University of New South Wales , Sydney, Australia to provide a platform from which astronomical observations and site-testing could be conducted. Various institutions from Australia, US, China and
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#1732772436362492-525: Is located near Adélie Land close to the ice sheet's southeast coast, at the Astrolabe Subglacial Basin , where it measured 4,897 m (16,066 ft) around 2013. Much of the ice sheet is already located at a high elevation: in particular, Dome Argus Plateau has an average height of around 4 km (2.5 mi), and yet it is underlain by the Gamburtsev Mountain Range , which has the average height of 2.7 km (1.7 mi) and
533-512: Is most likely to first see sustained losses of ice at its most vulnerable locations such as Totten Glacier and Wilkes Basin . Those areas are sometimes collectively described as East Antarctica's subglacial basins, and it is believed that once the warming reaches around 3 °C (5.4 °F), then they would start to collapse over a period of around 2,000 years, This collapse would ultimately add between 1.4 m (4 ft 7 in) and 6.4 m (21 ft 0 in) to sea levels, depending on
574-614: Is near one end of an elongate ridge (about 60 km (37 mi) long and 10 km (6.2 mi) wide), which is a major ice divide and has an elevation difference along its length of only a few meters. An automatic weather station (AWS) was deployed at Dome A, and a second station was installed approximately halfway between the summit and the coast at a site called Eagle ( 76°25′S 77°01′E / 76.417°S 77.017°E / -76.417; 77.017 , 2830 m above sea level). These AWS are operated as part of an ongoing collaboration between China and Australia and include
615-553: Is the highest ice feature in Antarctica , consisting of an ice dome or eminence 4,093 m (13,428 ft) above sea level. It is located near the center of East Antarctica , approximately midway between the enormous head of Lambert Glacier and the geographic South Pole , within the Australian claim . Dome Argus is located on the massive East Antarctic Ice Sheet and is the highest ice feature of Antarctica. Dome A
656-463: Is the only place on Earth cold enough for atmospheric temperature inversion to occur consistently. That is, while the atmosphere is typically warmest near the surface and becomes cooler at greater elevation, atmosphere during the Antarctic winter is cooler at the surface than in its middle layers. Consequently, greenhouse gases actually trap heat in the middle atmosphere and reduce its flow towards
697-604: Is too little annual precipitation to form an ice layer, which is the case in the so-called McMurdo Dry Valleys of the Southern Victoria Land . Another exception are the subglacial lakes , which occur so deep beneath the ice that the pressure melting point is well below 0 °C (32 °F). Many countries have made territorial claims in Antarctica . Within EAIS, the United Kingdom , France , Norway , Australia , Chile and Argentina all claim
738-547: The Argonauts traveled to Colchis in search of the Golden Fleece . This site is one of the driest locations on Earth and receives 1 to 3 cm (0.4 to 1.2 in) of snow per year. Due to this, as well as calm weather, this site is an excellent location to obtain ice core samples for the research of past climates . Temperatures at Dome A fall below −80 °C (−112 °F) almost every winter. Details of
779-671: The Earth's crust ) with the area of 10,200,000 km (3,900,000 sq mi), which accounts for around 73% of the entire Antarctic landmass. East Antarctica is separate from West Antarctica due to the presence of Transantarctic Mountains , which span nearly 3,500 km (2,200 mi) from the Weddell Sea to the Ross Sea , and have a width of 100–300 km (62–186 mi). The ice sheet has an average thickness of around 2.2 km (1.4 mi). The thickest ice in Antarctica
820-762: The Fimbulisen ice shelf in the Queen Maud Land . If global warming were to reach higher levels, then the EAIS would play an increasingly larger role in sea level rise occurring after 2100. According to the most recent reports of the Intergovernmental Panel on Climate Change ( SROCC and the IPCC Sixth Assessment Report ), the most intense climate change scenario , where the anthropogenic emissions increase continuously, RCP8.5 , would result in Antarctica alone losing
861-430: The ice sheet model used. Isostatic rebound of the newly ice-free land would also add 8 cm (3.1 in) and 57 cm (1 ft 10 in), respectively. The entire East Antarctic Ice Sheet holds enough ice to raise global sea levels by 53.3 m (175 ft). Its complete melting is also possible, but it would require very high warming and a lot of time: In 2022, an extensive assessment of tipping points in
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#1732772436362902-480: The ice sheet model used. The EAIS as a whole holds enough ice to raise global sea levels by 53.3 m (175 ft). However, it would take global warming in a range between 5 °C (9.0 °F) and 10 °C (18 °F), and a minimum of 10,000 years for the entire ice sheet to be lost. East Antarctic Ice Sheet is located directly above the East Antarctic Shield – a craton (stable area of
943-405: The Antarctic winter results in middle layers of the atmosphere being warmer than the surface. This leads to the negative greenhouse effect on a local scale, where greenhouse gases trap heat in the middle atmosphere and reduce its flow towards the surface and towards space, while normally, they prevent the flow of heat from the lower atmosphere and towards space. This effect lasts until the end of
984-531: The Antarctic winter. Consequently, East Antarctica had experienced cooling in the 1980s and 1990s, even as the rest of the Earth was warming. For instance, between 1986 and 2006 there had been a cooling of 0.7 °C (1.3 °F) per decade at Lake Hoare station in the McMurdo Dry Valleys . A 2002 paper by Peter Doran suggested that the cooling over East Antarctica outweighed warming of the rest of
1025-509: The UK provided instruments that were deployed with PLATO, these instruments included CSTAR, Gattini, PreHEAT, Snodar, Nigel and the PLATO web cameras. The Institute of Remote Sensing Applications, Chinese Academy of Sciences [1] established a wireless network technology based observation system called Dome A-WSN on the dome in January 2008. The Kunlun Station , China's third station in Antarctica,
1066-619: The book's claims. In 2009, it was demonstrated that the West Antarctic Ice Sheet has warmed by more than 0.1 °C/decade since the 1950s, resulting in a statistically significant warming trend across Antarctica of >0.05 °C/decade since 1957. Later research found that after 2000, the warming of West Antarctica locations slowed or partially reversed between 2000 and 2020, while the East Antarctica interior had demonstrated clear warming. This happened due to
1107-548: The climate system published in Science Magazine concluded that the ice sheet would take a minimum of 10,000 years to fully melt. It would most likely be committed to complete disappearance only once the global warming reaches about 7.5 °C (13.5 °F), with the minimum and the maximum range between 5 °C (9.0 °F) and 10 °C (18 °F). Another estimate suggested that at least 6 °C (11 °F) would be needed to melt two thirds of its volume. If
1148-464: The coldest continent, and East Antarctica is additionally cooler than the West Antarctica, because it is located at a substantially greater elevation. Thus, it is the only place on Earth cold enough for atmospheric temperature inversion to occur every winter. While the atmosphere on Earth is at its warmest near the surface and becomes cooler as elevation increases, temperature inversion during
1189-411: The continent. While the paper estimated that about 42% of the Antarctic area had been warming, it was wrongly described by many media outlets as a proof that there was no warming in Antarctica. In 2004, author Michael Crichton used that cooling as one of his arguments for denying climate change in his novel State of Fear . First other scientists, and then Peter Doran himself eventually had to debunk
1230-529: The entire ice sheet were to disappear, then the change in ice-albedo feedback would increase the global temperature by 0.6 °C (1.1 °F), while the regional temperatures would increase by around 2 °C (3.6 °F). The loss of the subglacial basins alone would only add about 0.05 °C (0.090 °F) to global temperatures due to their relatively limited area, and a correspondingly low impact on global albedo. 45th meridian west Download coordinates as: The meridian 45° west of Greenwich
1271-444: The global warming reaches 3 °C (5.4 °F) - the plausible temperature range is between 2 °C (3.6 °F) and 6 °C (11 °F). Then, the subglacial basins would gradually collapse over a period of around 2,000 years, although it may be as fast as 500 years or as slow as 10,000 years. Their loss would ultimately add between 1.4 m (4 ft 7 in) and 6.4 m (21 ft 0 in) to sea levels, depending on
East Antarctic Ice Sheet - Misplaced Pages Continue
1312-655: The local changes in Southern Annular Mode the dominant climate variability pattern over the Antarctica. Some of those changes were caused by the ozone layer beginning to recover following the Montreal Protocol . The limited warming and already low temperatures over East Antarctica mean that as of early 2020s, the majority of observational evidence shows it continuing to gain mass. Some analyses have suggested it already began to lose mass in 2000s, but they over-extrapolated some observed losses onto
1353-718: The morphology of this feature were determined by the SPRI-NSF-TUD airborne radio echo sounding program between the years 1967 and 1979. In January 2005 a team from the Chinese National Antarctic Research Expeditions (CHINARE) traversed 1,228 km (763 mi) from Zhongshan Station to Dome A and located the highest point of the ice sheet (4,093 m (13,428 ft) above sea level) by GPS survey at 80°22′S 77°21′E / 80.367°S 77.350°E / -80.367; 77.350 on January 18. This point
1394-554: The past 8 million years. While it had still thinned by at least 500 m (1,600 ft) during the Pleistocene period, and by less than 50 m (160 ft) since Last Glacial Maximum , the land area covered by ice in East Antarctica remained largely the same. Contrastingly, the smaller West Antarctic ice sheet is thought to have largely collapsed as recently as during the Eemian period, about 125,000 years ago. Antarctica as
1435-412: The poorly-observed areas, and a more complete observational record shows continued mass gain. Because it is currently gaining mass, East Antarctic Ice Sheet is not expected to play a role in the 21st century sea level rise . However, it is still subject to adverse change, such as the retreat of Denman Glacier , or the flow of warmer ocean current into ice cavities beneath the stabilizing ice shelves like
1476-627: The rest of the continent was frequently misinterpreted by the media and occasionally used as an argument for climate change denial . After 2009, improvements in Antarctica's instrumental temperature record have proven that the warming over West Antarctica resulted in consistent net warming across the continent since the 1957. Because the East Antarctic ice sheet has barely warmed, it is still gaining ice on average. for instance, GRACE satellite data indicated East Antarctica mass gain of 60 ± 13 billion tons per year between 2002 and 2010. It
1517-542: The sea level. Evidence from the Pleistocene shows that Wilkes Basin had likely lost enough ice to add 0.5 m (1 ft 8 in) to sea levels between 115,000 and 129,000 years ago, during the Eemian , and about 0.9 m (2 ft 11 in) between 318,000 and 339,000 years ago, during the Marine Isotope Stage 9 . Neither Wilkes nor the other subglacial basins were lost entirely, but estimates suggest that they would be committed to disappearance once
1558-416: The surface while the temperature inversion lasts. Due to these factors, East Antarctica had experienced slight cooling for decades while the rest of the world warmed as the result of climate change . Clear warming over East Antarctica only started to occur since the year 2000, and was not conclusively detected until the 2020s. In the early 2000s, cooling over East Antarctica seemingly outweighing warming over
1599-501: The warming were to remain at elevated levels for a long time, then the East Antarctic Ice Sheet would eventually become the dominant contributor to sea level rise, simply because it contains the largest amount of ice. Sustained ice loss from the EAIS would begin with the significant erosion of the so-called subglacial basins, such as Totten Glacier and Wilkes Basin , which are located in vulnerable locations below
1640-594: Was initially unstable, and did not grow to consistently cover the entire continent until 32.8 million years ago, when the CO 2 levels had further declined to below 600 ppm. Afterwards, the East Antarctic Ice Sheet declined substantially during the Middle Miocene Climatic Optimum 15 million years ago, yet started to recover about 13.96 million years ago. Since then, it had been largely stable, experiencing "minimal" change in its surface extent over
1681-525: Was −82.5 °C (−116.5 °F) in July 2005. This may have been beaten by an unconfirmed reading of −82.7 °C (−116.9 °F) in June 2019. The lowest surface temperature ever measured on the surface of the Earth (−93.2 °C (−135.8 °F)) was recorded by satellite on August 10, 2010, between Dome Argus and Dome Fuji . Analysis of satellite data and atmospheric models shows that Ridge A , which