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Climate of Antarctica

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The climate of Antarctica is the coldest on Earth. The continent is also extremely dry (it is a desert[1]), averaging 166 mm (6.5 in) of precipitation per year. Snow rarely melts on most parts of the continent, and, after being compressed, becomes the glacier ice that makes up the ice sheet. Weather fronts rarely penetrate far into the continent, because of the katabatic winds. Most of Antarctica has an ice-cap climate (Köppen classification EF) with extremely cold and dry weather.

Surface temperature of Antarctica in winter and summer from the European Centre for Medium-Range Weather Forecasts

Temperature

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The highest temperature ever recorded on Antarctica was 19.8 °C (67.6 °F) recorded at Signy Research Station, Signy Island on 30 January 1982.[2][3]

The highest temperature on the Antarctic mainland was 18.3 °C (64.9 °F) at the Esperanza Base (Argentina) on 6 February 2020.[4]

 
The Antarctic temperature changes during the last several glacial and interglacial cycles of the present ice age

The lowest air temperature record, the lowest reliably measured temperature on Antarctica was set on 21 July 1983, when a temperature of −89.2 °C (−128.6 °F) was observed at Vostok Station.[2][5] For comparison, this is 10.7 °C (19.3 °F) colder than subliming dry ice (at sea level pressure). The elevation of the location is 3,488 meters (11,444 feet).

Satellite measurements have identified even lower ground temperatures, with −93.2 °C (−135.8 °F) having been observed at the cloud-free East Antarctic Plateau on 10 August 2010.[6]

The lowest recorded temperature of any location on Earth's surface at 81°48′S 63°30′E / 81.8°S 63.5°E / -81.8; 63.5 was revised with new data in 2018 in nearly 100 locations, ranging from −93.2 °C (−135.8 °F)[7] to −98 °C (−144.4 °F).[8] This unnamed part of the Antarctic plateau, between Dome A and Dome F, was measured on 10 August 2010, and the temperature was deduced from radiance measured by the Landsat 8 and other satellites. It was discovered during a National Snow and Ice Data Center review of stored data in December 2013[9] but revised by researchers on 25 June 2018.[10][11] This temperature is not directly comparable to the –89.2 °C reading quoted above, since it is a skin temperature deduced from satellite-measured upwelling radiance, rather than a thermometer-measured temperature of the air 1.5 m (5 ft) above the ground surface.

The mean annual temperature of the interior is −43.5 °C (−46.3 °F).[12] The coast is warmer; on the coast Antarctic average temperatures are around −10 °C (14.0 °F) (in the warmest parts of Antarctica) and in the elevated inland they average about −55 °C (−67.0 °F) in Vostok.[13][14] Monthly means at McMurdo Station range from −26 °C (−14.8 °F) in August to −3 °C (26.6 °F) in January.[15] At the South Pole, the highest temperature ever recorded was −12.3 °C (9.9 °F) on 25 December 2011.[16] Along the Antarctic Peninsula, temperatures as high as 18.3 °C (64.9 °F) have been recorded,[clarification needed] though the summer temperature is below 0 °C (32 °F) most of the time. Severe low temperatures vary with latitude, elevation, and distance from the ocean. East Antarctica is colder than West Antarctica because of its higher elevation.[citation needed] The Antarctic Peninsula has the most moderate climate. Higher temperatures occur in January along the coast and average slightly below freezing.

Precipitation

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Map of average annual precipitation on Antarctica (mm liquid equivalent)

The total precipitation on Antarctica, averaged over the entire continent, is about 166 millimetres (6.5 inches) per year (Vaughan et al., J. Clim., 1999). The actual rates vary widely, from high values over the Peninsula (380 to 640 millimetres (15 to 25 inches) a year) to very low values (as little as 50 millimetres (2.0 inches) in the high interior (Bromwich, Reviews of Geophysics, 1988). Areas that receive less than 250 millimetres (9.8 inches) of precipitation per year are classified as deserts. Almost all Antarctic precipitation falls as snow.[17] Rainfall is rare and mainly occurs during the summer in coastal areas and surrounding islands.[17] Note that the quoted precipitation is a measure of its equivalence to water, rather than being the actual depth of snow. The air in Antarctica is also very dry. The low temperatures result in a very low absolute humidity, which means that dry skin and cracked lips are a continual problem for scientists and expeditioners working on the continent.[18]

Weather condition classification

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Main article: Antarctica Weather Danger Classification

The weather in Antarctica can be highly variable, and the weather conditions can often change dramatically in short periods of time. There are various classifications for describing weather conditions in Antarctica; restrictions given to workers during the different conditions vary by station and nation.[19][20][21]

Ice cover

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Nearly all of Antarctica is covered by a sheet of ice that is, on average, at least 1,500 m (5,000 ft) thick. Antarctica contains 90% of the world's ice and more than 70% of its fresh water. If all the land-ice covering Antarctica were to melt — around 30×10^6 km3 (7.2×10^6 cu mi) of ice — the seas would rise by over 60 m (200 ft).[22] The Antarctic is so cold that even with increases of a few degrees, temperatures would generally remain below the melting point of ice. Higher temperatures are expected to lead to more precipitation, which takes the form of snow. This would increase the amount of ice in Antarctica, offsetting approximately one third of the expected sea level rise from thermal expansion of the oceans.[23] During a recent[when?] decade, East Antarctica thickened at an average rate of about 1.8 cm (11⁄16 in) per year while West Antarctica showed an overall thinning of 0.9 cm (3⁄8 in) per year.[24] For the contribution of Antarctica to present and future sea level change, see sea level rise. Because ice flows, albeit slowly, the ice within the ice sheet is younger than the age of the sheet itself.

Morphometric data for Antarctica (from Drewry, 1983)
Surface Area
(km²) 		Percent Mean ice thickness
(m) 		Volume
(km3) 		Percent
Inland ice sheet 11,965,700 85.97 2,450 29,324,700 97.00
Ice shelves 1,541,710 11.08 475 731,900 2.43
Ice rises 78,970 .57 670 53,100 .18
Glacier ice (total) 13,586,380   2,160 30,109,800¹
Rock outcrop 331,690 2.38
Antarctica (total) 13,918,070 100.00 2,160 30,109,800¹ 100.00
¹The total ice volume is different from the sum of the component parts because individual figures have been rounded.
Regional ice data (from Drewry and others, 1982; Drewry, 1983)
Region Area
(km²) 		Mean ice
thickness
(m) 		Volume
(km3)
East Antarctica
Inland ice 9,855,570 2,630 25,920,100
Ice shelves 293,510 400 117,400
Ice rises 4,090 400 1,600
West Antarctica (excluding Antarctic Peninsula)
Inland ice sheet 1,809,760 1,780 3,221,400
Ice shelves 104,860 375 39,300
Ice rises 3,550 375 1,300
Antarctic Peninsula
Inland ice sheet 300,380 610 183,200
Ice shelves 144,750 300 43,400
Ice rises 1,570 300 500
Ross Ice Shelf
Ice shelf 525,840 427 224,500
Ice rises 10,320 500 5,100
Filchner-Ronne Ice Shelf
Ice shelf 472,760 650 307,300
Ice rises 59,440 750 44,600

Ice shelves

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Antarctic ice shelves, 1998

About 75% of the coastline of Antarctica is ice shelf. The majority of ice shelf consists of floating ice, and a lesser amount consists of glaciers that move slowly from the land mass into the sea. Ice shelves lose mass through breakup of glacial ice (calving), or basal melting due to warm ocean water under the ice.[25]

Melting or breakup of floating shelf ice does not directly affect global sea levels; however, ice shelves have a buttressing effect on the ice flow behind them. 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.
  • Parts of the Larsen Ice Shelf broke up in recent decades.
    • 1995: The Larsen A ice shelf disintegrated in January 1995.
    • 2001: 3,250 km2 (1,250 sq mi) of the Larsen B ice shelf disintegrated in February 2001. It had been gradually retreating before the breakup event.
    • 2015: A study concluded that the remaining Larsen B ice-shelf will disintegrate by the end of the decade, based on observations of faster flow and rapid thinning of glaciers in the area.[26]

The George VI Ice Shelf, which may be on the brink of instability,[27] has probably existed for approximately 8,000 years, after melting 1,500 years earlier.[28] Warm ocean currents may have been the cause of the melting.[29] Not only are the ice sheets losing mass, they are losing mass at an accelerating rate.[30]

Climate change

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This section is an excerpt from Climate change in Antarctica.[edit]

Climate change caused by greenhouse gas emissions from human activities occurs everywhere on Earth, and while Antarctica is less vulnerable to it than any other continent,[31] climate change in Antarctica has been observed. Since 1959, there has been an average temperature increase of >0.05 °C/decade since 1957 across the continent, although it had been uneven.[32] West Antarctica warmed by over 0.1 °C/decade from the 1950s to the 2000s, and the exposed Antarctic Peninsula has warmed by 3 °C (5.4 °F) since the mid-20th century.[33] The colder, stabler East Antarctica had been experiencing cooling until the 2000s.[34][35] Around Antarctica, the Southern Ocean has absorbed more oceanic heat than any other ocean,[36] and has seen strong warming at depths below 2,000 m (6,600 ft).[37]: 1230  Around the West Antarctic, the ocean has warmed by 1 °C (1.8 °F) since 1955.[33]

The warming of the Southern Ocean around Antarctica has caused the weakening or collapse of ice shelves, which float just offshore of glaciers and stabilize them. Many coastal glaciers have been losing mass and retreating, causing net-annual ice loss across Antarctica,[37]: 1264  although the East Antarctic ice sheet continues to gain ice inland. By 2100, net ice loss from Antarctica is expected to add about 11 cm (5 in) to global sea level rise. Marine ice sheet instability may cause West Antarctica to contribute tens of centimeters more if it is triggered before 2100.[37]: 1270  With higher warming, instability would be much more likely, and could double global, 21st-century sea-level rise.[38][39][40]

See also

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References

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Notes

  1. ^ "Frequently Asked Questions about Antarctica". nasa.gov. NASA. Retrieved 5 May 2024.
  2. ^ a b "WMO verifies highest temperatures for Antarctic Region". 1 March 2017. Archived from the original on 18 December 2023. Retrieved 12 July 2018.
  3. ^ "WMO verifies one temperature record for Antarctic continent and rejects another". World Meteorological Organization. 1 July 2021. Retrieved 3 July 2021.
  4. ^ "WMO verifies one temperature record for Antarctic continent and rejects another". The World Meteorological Organization (WMO). 1 July 2021. Retrieved 17 May 2022.
  5. ^ "World: Lowest Temperature - ASU World Meteorological Organization". asu.edu. Archived from the original on 16 June 2010.
  6. ^ Coldest spot on Earth identified by satellite Archived 14 April 2016 at the Wayback Machine, Jonathan Amos, BBC News, 9 December 2013.
  7. ^ Natasha Vizcarra (9 December 2013). "Landsat 8 helps unveil the coldest place on Earth". National Snow and Ice Data Center. Archived from the original on 20 December 2013. Retrieved 27 December 2013.
  8. ^ Natasha Vizcarra (25 May 2018). "New study explains Antarctica's coldest temperatures". The National Snow and Ice Data Center (NSIDC). Archived from the original on 5 March 2021. Retrieved 7 August 2018.
  9. ^ Jonathan Amos (9 December 2013). "Coldest spot on Earth identified by satellite". BBC News Science & Environment. Archived from the original on 26 December 2013. Retrieved 27 December 2013.
  10. ^ Ted Scambos (25 May 2018). "Scambros et al 2018" (PDF). The National Snow and Ice Data Center (NSIDC).
  11. ^ NOT CORRECTED. "BBC Corrections and Clarifications page". Archived from the original on 13 October 2018. Retrieved 7 August 2018.
  12. ^ "Annual mean 2m Temperature for 0-150ºE, 75-90ºS, Climate Reanalyzer". Climate Change Institute, University of Maine. Retrieved 18 May 2023.
  13. ^ "Antarctic weather". www.antarctica.gov.au. Archived from the original on 5 November 2016.
  14. ^ "Antarctic climatic data". Archived from the original on 7 May 2008. Retrieved 7 May 2008.
  15. ^ "Antarctica Climate data and graphs, South Pole, McMurdo and Vostok". coolantarctica.com. Archived from the original on 9 October 2010. Retrieved 14 May 2014.
  16. ^ Matthew A. Lazzara (28 December 2011). "Preliminary Report: Record Temperatures at South Pole (and nearby AWS sites…)". Archived from the original on 30 December 2011. Retrieved 28 December 2011.
  17. ^ a b "La Antártida" (in Spanish). Dirección Nacional del Antártico. Archived from the original on 13 November 2016. Retrieved 13 November 2016.
  18. ^ "Is Mainstream Tourism a Good Way to Save Helpless Antarctica?". Fair Observer. Retrieved 9 July 2024.
  19. ^ "Weathering The Conditions" (PDF). The Antarctic Sun. 18 October 1997. p. 8. Archived (PDF) from the original on 9 June 2015. Retrieved 8 June 2015.
  20. ^ Jim Scott. "Weather and Travel" (PDF). Welcome to McMurdo Station. McMurdo Station. p. 6. Archived from the original (PDF) on 10 September 2014. Retrieved 8 June 2015.
  21. ^ "Field Manual" (PDF). Antarctica New Zealand. New Zealand Government. p. 37. Archived from the original (PDF) on 15 January 2015. Retrieved 8 June 2015.
  22. ^ "Climate Change 2001: The Scientific Basis". Grida.no. Archived from the original on 16 December 2007. Retrieved 27 March 2011.
  23. ^ "Climate Change 2001: The Scientific Basis". Grida.no. Archived from the original on 14 May 2011. Retrieved 27 March 2011.
  24. ^ Davis CH, Li Y, McConnell JR, Frey MM, Hanna E (2005). "Snowfall-Driven Growth in East Antarctic Ice Sheet Mitigates Recent Sea-Level Rise". Science. 308 (5730): 1898–1901. Bibcode:2005Sci...308.1898D. doi:10.1126/science.1110662. PMID 15905362. S2CID 31797055.
  25. ^ E. Rignot; S. Jacobs; J. Mouginot; B. Scheuchl (2013). "Ice-Shelf Melting Around Antarctica". Science. 341 (6143): 266–270. Bibcode:2013Sci...341..266R. doi:10.1126/science.1235798. PMID 23765278. S2CID 206548095.
  26. ^ NASA (14 May 2015). "NASA Study Shows Antarctica's Larsen B Ice Shelf Nearing Its Final Act". Archived from the original on 9 June 2015.
  27. ^ Bentley, Mike; Hodgson, Dominic. "Millennial-scale variability of George VI Ice Shelf, Antarctic Peninsula". Natural Environment Research Council. Archived from the original on 12 September 2002. Retrieved 8 June 2015.
  28. ^ Bentley, M.J.; Hjort, C.; Ingolfsson, O.; Sugden, D.E. "Holocene Instability of the George VI Ice Shelf, Antarctic Peninsula". Archived from the original on 20 October 2004. Retrieved 8 June 2015.
  29. ^ "Press Release – New Year's Honours for British Antarctic Survey Personnel". British Antarctic Survey. 5 January 2006. Archived from the original on 15 December 2006.
  30. ^ "NASA - Is Antarctica Melting?". www.nasa.gov. Archived from the original on 12 December 2016.
  31. ^ Singh, Hansi A.; Polvani, Lorenzo M. (10 January 2020). "Low Antarctic continental climate sensitivity due to high ice sheet orography". npj Climate and Atmospheric Science. 3 (1): 39. Bibcode:2020npCAS...3...39S. doi:10.1038/s41612-020-00143-w. S2CID 222179485.
  32. ^ Steig, Eric; Schneider, David; Rutherford, Scott; Mann, Michael E.; Comiso, Josefino; Shindell, Drew (1 January 2009). "Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year". Arts & Sciences Faculty Publications.
  33. ^ a b "Impacts of climate change". Discovering Antarctica. Retrieved 15 May 2022.
  34. ^ Clem, Kyle R.; Fogt, Ryan L.; Turner, John; Lintner, Benjamin R.; Marshall, Gareth J.; Miller, James R.; Renwick, James A. (August 2020). "Record warming at the South Pole during the past three decades". Nature Climate Change. 10 (8): 762–770. Bibcode:2020NatCC..10..762C. doi:10.1038/s41558-020-0815-z. ISSN 1758-6798. S2CID 220261150.
  35. ^ Xin, Meijiao; Clem, Kyle R; Turner, John; Stammerjohn, Sharon E; Zhu, Jiang; Cai, Wenju; Li, Xichen (2 June 2023). "West-warming East-cooling trend over Antarctica reversed since early 21st century driven by large-scale circulation variation". Environmental Research Letters. 18 (6): 064034. doi:10.1088/1748-9326/acd8d4.
  36. ^ Bourgeois, Timothée; Goris, Nadine; Schwinger, Jörg; Tjiputra, Jerry F. (17 January 2022). "Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S". Nature Communications. 13 (1): 340. Bibcode:2022NatCo..13..340B. doi:10.1038/s41467-022-27979-5. PMC 8764023. PMID 35039511.
  37. ^ a b c 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, USA: 1270–1272.
  38. ^ Nauels, Alexander; Rogelj, Joeri; Schleussner, Carl-Friedrich; Meinshausen, Malte; Mengel, Matthias (1 November 2017). "Linking sea level rise and socioeconomic indicators under the Shared Socioeconomic Pathways". Environmental Research Letters. 12 (11): 114002. Bibcode:2017ERL....12k4002N. doi:10.1088/1748-9326/aa92b6. hdl:20.500.11850/230713.
  39. ^ L. Bamber, Jonathan; Oppenheimer, Michael; E. Kopp, Robert; P. Aspinall, Willy; M. Cooke, Roger (May 2019). "Ice sheet contributions to future sea-level rise from structured expert judgment". Proceedings of the National Academy of Sciences. 116 (23): 11195–11200. Bibcode:2019PNAS..11611195B. doi:10.1073/pnas.1817205116. PMC 6561295. PMID 31110015.
  40. ^ Horton, Benjamin P.; Khan, Nicole S.; Cahill, Niamh; Lee, Janice S. H.; Shaw, Timothy A.; Garner, Andra J.; Kemp, Andrew C.; Engelhart, Simon E.; Rahmstorf, Stefan (8 May 2020). "Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey". npj Climate and Atmospheric Science. 3 (1): 18. Bibcode:2020npCAS...3...18H. doi:10.1038/s41612-020-0121-5. hdl:10356/143900. S2CID 218541055.

Sources

Further reading

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Main article: Bibliography of Antarctica
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Climate

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Climate change in Antarctica

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Antarctic ice

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