Global warming hitting all of Antarctica: scientistsScientists on Wednesday unveiled evidence to suggest global warming global warming, the gradual increase of the temperature of the earth's lower atmosphere as a result of the increase in greenhouse gases since the Industrial Revolution. is affecting all of Antarctica, home to the world's mightiest store of ice. The average temperature across the White Continent has been rising for the last half century and the finger of blame points at the greenhouse effect greenhouse effect: see global warming. greenhouse effect Warming of the Earth's surface and lower atmosphere caused by water vapour, carbon dioxide, and other trace gases in the atmosphere. Visible light from the Sun heats the Earth's surface. , they said. The research, published in the British journal Nature, takes a fresh look at one of the great unknowns -- and dreads dreads pl.n. Informal Dreadlocks. -- in climate science. Any significant thaw of Antarctica could drown many coastal cities and delta regions. Bigger than Australia, Antarctica holds enough ice to raise global sea levels by 57 metres (185 feet). Previous monitoring has already pinpointed the Antarctic Peninsula Antarctic Peninsula, glaciated mountain region of W Antarctica, extending c.1,200 mi (1,930 km) N toward South America; in the south, volcanic peaks rise to c.11,000 ft (3,350 m). Most of its NE coast is fringed by the Larsen ice shelf. -- the tongue that juts 800 kilometres (500 miles) towards South America South America, fourth largest continent (1991 est. pop. 299,150,000), c.6,880,000 sq mi (17,819,000 sq km), the southern of the two continents of the Western Hemisphere. -- as a "hotspot" where hundreds of glaciers have been in retreat since the start of the decade. But until now the news has been reassuring regarding Antarctica's two massive icesheets. Indeed, a common belief is that the icy slabs have even cooled slightly and possibly thickened thick·en tr. & intr.v. thick·ened, thick·en·ing, thick·ens 1. To make or become thick or thicker: Thicken the sauce with cornstarch. The crowd thickened near the doorway. 2. , partly in response to the chilling seasonal effects of the ozone hole ozone hole n. An area of the ozone layer, such as the large area over Antarctica or the smaller area over the North Pole, that periodically becomes depleted of ozone. over the South Pole South Pole, southern end of the earth's axis, lat. 90° S. It is distinguished from the south magnetic pole. The South Pole was reached by Roald Amundsen, a Norwegian explorer, in 1911. See Antarctica. . Not so, the new study says. It calculates that West Antarctica West Antarctica, or Lesser Antarctica (), is one of the two major regions of Antarctica, lying on the Pacific Ocean side of the Transantarctic Mountains and comprising Marie Byrd Land, Ellsworth Land, and Antarctic Peninsula. has been warming by 0.17 degrees Celsius (0.3 degrees Fahrenheit) per decade over the past 50 years. This is even more than the Peninsula, where the average rise is estimated as 0.11 C (0.2 F) per decade. There has indeed been some cooling in East Antarctica East Antarctica, also called Greater Antarctica, is one of the two major regions of Antarctica, lying on the Indian Ocean side of the Transantarctic Mountains and comprising Coats Land, Queen Maud Land, Enderby Land, Mac. Robertson Land, Wilkes Land and Victoria Land. , but this was mainly in the autumn, and occurred as a result of the ozone hole. There was also a period of strong cooling between 1970 and 2000. But, overall and when calculated over 50 years, East Antarctica has warmed too -- by an average of 0.1 C (0.18 F) per decade, a figure that the authors describe as "significant". "The sense of 'Oh, it's cooling in East Antarctica,' is based essentially on the 1970-2000 period, and it's warmed since then -- although we don't have a lot of data for the most recent period -- and it definitely warmed prior to the 1970s," Eric Steig, a professor of Earth and space sciences at the University of Washington, told AFP (1) (AppleTalk Filing Protocol) The file sharing protocol used in an AppleTalk network. In order for non-Apple networks to access data in an AppleShare server, their protocols must translate into the AFP language. See file sharing protocol. . "When you look at the big picture on that, the average [trend in East Antarctica] is actually warming." Put together, the average temperature rise for Antarctica is put at 0.12 C (0.22 F) per decade, the study said. The work is based on a 25-year archive of observations by satellites measuring the intensity of infrared light radiated by the snow pack. These were buttressed by data from automated weather stations deployed around the Antarctic coast since 1957. The paper does not venture any estimate about ice loss or predict the icesheets' stability, but says only global warming can logically explain the temperature trend. "This shouldn't cause anyone to worry more than they did before. But what it does do is kill off the rather silly and careless statements out there from some people to the effect that Antarctica's cooling," said Steig. Such comments "put into question all the other science that supports the idea that there is warming and it's human beings' fault," he said. There could be bad news a few decades down the road, when efforts to fix the ozone hole bear fruit, added Steig. "The hole could be eliminated by the middle of this century. If that happens, all of Antarctica could begin warming on a par with the rest of the world," he warned. The West Antarctic icesheet, which holds enough ice to boost global sea levels by up to six metres (19.5 feet), lies at an average height of about 1,800 metres (6,000 feet). The East Antarctic icesheet, divided from West Antarctica by a mountain chain, has an average elevation of around 3,000 metres (10,000 feet), which makes it not only bigger but also colder. If it melted in its entirety -- something that most scientists discount except only as a very distant doomsday scenario -- today's coastlines would be drowned to a height of 50 metres (165 feet).
|
|
||||||||||||||||

Printer friendly
Cite/link
Email
Feedback
Reader Opinion