Английская Википедия:Climate of Antarctica
Шаблон:Use dmy dates Шаблон:Short description
The climate of Antarctica is the coldest on Earth. The continent is also extremely dry (it is a desert), averaging Шаблон:Convert 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.
Temperature
The highest temperature ever recorded on Antarctica was Шаблон:Convert recorded at Signy Research Station, Signy Island on 30 January 1982.[1][2]
The highest temperature on the Antarctic mainland was Шаблон:Convert at the Esperanza Base (Argentina) on 6 February 2020.[3]
The lowest air temperature record, the lowest reliably measured temperature on Antarctica was set on 21 July 1983, when a temperature of Шаблон:Convert was observed at Vostok Station.[1][4] For comparison, this is Шаблон:Convert colder than subliming dry ice (at sea level pressure). The elevation of the location is Шаблон:Convert.
Satellite measurements have identified even lower ground temperatures, with Шаблон:Convert having been observed at the cloud-free East Antarctic Plateau on 10 August 2010.[5]
The lowest recorded temperature of any location on Earth's surface at Шаблон:Coord was revised with new data in 2018 in nearly 100 locations, ranging from Шаблон:Convert[6] to Шаблон:Convert.[7] 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[8] but revised by researchers on 25 June 2018.[9][10] 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 Шаблон:Convert above the ground surface.
The mean annual temperature of the interior is Шаблон:Convert.[11] The coast is warmer; on the coast Antarctic average temperatures are around Шаблон:Convert (in the warmest parts of Antarctica) and in the elevated inland they average about Шаблон:Convert in Vostok.[12][13] Monthly means at McMurdo Station range from Шаблон:Convert in August to Шаблон:Convert in January.[14] At the South Pole, the highest temperature ever recorded was Шаблон:Convert on 25 December 2011.[15] Along the Antarctic Peninsula, temperatures as high as Шаблон:Convert have been recorded,Шаблон:Clarify though the summer temperature is below Шаблон:Convert 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.Шаблон:Citation needed The Antarctic Peninsula has the most moderate climate. Higher temperatures occur in January along the coast and average slightly below freezing.
Precipitation
The total precipitation on Antarctica, averaged over the entire continent, is about Шаблон:Convert per year (Vaughan et al., J. Clim., 1999). The actual rates vary widely, from high values over the Peninsula (15 to 25 inches a year) to very low values (as little as Шаблон:Convert in the high interior (Bromwich, Reviews of Geophysics, 1988). Areas that receive less than Шаблон:Convert of precipitation per year are classified as deserts. Almost all Antarctic precipitation falls as snow.[16] Rainfall is rare and mainly occurs during the summer in coastal areas and surrounding islands.[16] 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.
Weather condition classification
Шаблон:Main 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.[17][18][19]
Ice cover
Nearly all of Antarctica is covered by a sheet of ice that is, on average, at least Шаблон:Convert 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 Шаблон:Convert of ice — the seas would rise by over Шаблон:Convert.[20] 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.[21] During a recentШаблон:When decade, East Antarctica thickened at an average rate of about Шаблон:Convert per year while West Antarctica showed an overall thinning of Шаблон:Convert per year.[22] 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.
| 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. | |||||
| 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
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.[23]
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: Шаблон:Convert 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.[24]
The George VI Ice Shelf, which may be on the brink of instability,[25] has probably existed for approximately 8,000 years, after melting 1,500 years earlier.[26] Warm ocean currents may have been the cause of the melting.[27] Not only are the ice sheets losing mass, they are losing mass at an accelerating rate.[28]
Climate change
See also
- Antarctic oscillation
- Antarctica cooling controversy
- Climate of the Arctic
- Effects of global warming
- Polar amplification
- Retreat of glaciers since 1850
- Southern Ocean
References
Notes Шаблон:Reflist
Sources
Further reading
- Warm Snap Turned Antarctica Green Around the Edges; Thawed-out continent was lined with trees 15 million years ago, study says. 20 June 2012 National Geographic
- Taking Antarctica's temperature; Frozen continent may not be immune to global warming 27 July 2013; Vol.184 #2 Science News
External links
Climate
- Temperature data from the READER project
- A pamphlet about the weather and climate of Antarctica
- Antarctica's central ice cap grows while glaciers melt
- Шаблон:Cite web
- Antarctica Climate and Weather
Climate change in Antarctica
- Western Antarctica warming confirmed 23 December 2012 USA Today
- NASA experts explain ice melt in Antarctica (2014)
Antarctic ice
- ↑ 1,0 1,1 Шаблон:Cite web
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- ↑ Coldest spot on Earth identified by satellite Шаблон:Webarchive, Jonathan Amos, BBC News, 9 December 2013.
- ↑ Шаблон:Cite web
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- ↑ 16,0 16,1 Шаблон:Cite web
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- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
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- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
