Major Deserts of the World
Major Deserts of the World : Antarctica
| Arabian | Atacama
| Chihuahuan | Gobi
| Great Basin | Great
Victoria | Highlands
of Iceland | Kalahari
| Monte | Patagonian
| Sahara | Taklamakan
| Thar
Antarctica Desert
Antarctica is Earth's southernmost continent, overlying the South Pole. Situated in the southern hemisphere and largely south of the Antarctic Circle, Antarctica is surrounded by the Southern Ocean. At 14.4 million km², it is the fifth-largest continent in area after Asia, Africa, North America, and South America; in turn, Europe and Australia are smaller. Some 98% of Antarctica is covered by ice, which averages at least 1.6 km in thickness.
On average, Antarctica is the coldest, driest and windiest continent, and has the highest average elevation of all the continents. Since there is little precipitation, except at the coasts, the interior of the continent is technically the largest desert in the world. There are no permanent human residents and Antarctica has never had an indigenous population. Only cold-adapted plants and animals survive there, including penguins, fur seals, mosses, lichens, and many types of algae.
Climate
Antarctica is the coldest place on Earth. It is a frozen desert
with little precipitation; the South Pole itself receives less
than 10 cm (4 inches) per year, on average. Temperatures reach
a minimum of between -80 °C and -90 °C (-112 °F and -130 °F) in
the interior in winter and reach a maximum of between +5 °C and
+15 °C (41 °F and 59 °F) near the coast in summer. Sunburn is
often a health issue as the snow surface reflects almost all of
the ultraviolet light falling on it. Eastern Antarctica is colder
than its western counterpart because of its higher elevation.
Weather fronts rarely penetrate far into the continent, leaving
the center cold and dry. Despite the lack of precipitation over
the central portion of the continent, ice there lasts for extended
time periods. Heavy snowfalls are not uncommon on the coastal
portion of the continent, where snowfalls of up to 1.22 meters
(48 inches) in 48 hours have been recorded.
At the edge of the continent, strong katabatic winds off the polar
plateau often blow at storm force. In the interior, however, wind
speeds are typically moderate. During summer, more solar radiation
reaches the surface during clear days at the South Pole than at
the equator because of the 24 hours of sunlight each day at the
Pole.
Antarctica is colder than the Arctic for two reasons. First, much of the continent is more than 3 km above sea level, and temperature decreases with elevation. Second, the Arctic Ocean covers the north polar zone: the ocean's relative warmth is transferred through the icepack and prevents temperatures in the Arctic regions from reaching the extremes typical of the land surface of Antarctica.
Given the latitude, long periods of constant darkness or constant
sunlight create climates unfamiliar to human beings in much of
the rest of the world. The aurora australis, commonly known as
the southern lights, is a glow observed in the night sky near
the South Pole. Another unique spectacle is diamond dust, a ground-level
cloud composed of tiny ice crystals. It generally forms under
otherwise clear or nearly clear skies, so people sometimes also
refer to it as clear-sky precipitation. A sun dog, a frequent
atmospheric optical phenomenon, is a bright "spot" beside the
true sun.
|
|
| |
Antarctia From Space
Art Print
Buy at AllPosters.com
Misty Mountains at Antarctic Circle
Photographic Print
Cardozo, Yvette
Buy at AllPosters.com
Ice Floes, Southern Ocean, off the Coast of Wilkes, Near Casey Station, Wilkes Land, Antarctica
Photographic Print
Dixon, Grant
Buy at AllPosters.com
Wind-Scoured Snow, Law Dome, Inland from Australia's Casey Station, Wilkes Land, Antarctica
Photographic Print
Dixon, Grant
Buy at AllPosters.com
|
|
 |
|