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From Wikipedia, the free encyclopedia

Polar desert with ground pattern characteristic of freeze-thaw alternation[citation needed]

Polar deserts are the regions of Earth that fall under an ice cap climate (EF under the Köppen classification). Despite rainfall totals low enough to normally classify as a desert, polar deserts are distinguished from true deserts (BWh or BWk under the Köppen classification) by low annual temperatures and evapotranspiration. Most polar deserts are covered in ice sheets, ice fields, or ice caps, and they are also called white deserts.[1]

Polar deserts are one of two polar biomes, the other being Arctic tundra. These biomes are located at the poles of Earth, covering much of the Antarctic in the southern hemisphere, and in the northern hemisphere extending from the Arctic into North America, Europe and Asia. Unlike the tundra that can support plant and animal life in the summer, polar deserts are largely barren environments, comprising permanent, flat layers of ice;[2] due to the scarcity of liquid water, the same is also true of the few ice-free areas. However, there is evidence of some life in this seemingly inhospitable landscape: sediments of organic and inorganic substances in the thick ice hosting microbial organisms closely related to cyanobacteria, able to fix carbon dioxide from the melting water.[3]

Temperature changes in polar deserts frequently cross the freezing point of water. This "freeze-thaw" alternation forms patterned textures on the ground, as much as 5 m (16 ft) in diameter.

Most of the interior of Antarctica is polar desert, despite the thick ice cover. Conversely, the McMurdo Dry Valleys of Antarctica, although they have had no ice for thousands of years due to katabatic wind but contain ephemeral streams and hypersaline lakes characteristic of extreme non-polar deserts, are not necessarily polar desert.[citation needed]

Polar deserts are relatively common during ice ages, as ice ages tend to be dry.[citation needed]

Climate scientists have voiced concerns about the effects of global warming to the ice poles in these polar biomes.[citation needed]

Effects and transpiration on climate

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Transcription

On our planet, we have two polar regions: the Arctic, whose name comes from the Greek Arktikos, of the North, and the Antarctic from Antarktikos, opposite of the North. But there's an easier way to remember them if you just remember what surrounds them. The Arctic, situated in the Northern hemisphere of our planet, is an ocean entirely surrounded by land. On the other side of the world, the Antarctic is a continent entirely surrounded by ocean. So, the Arctic has polar bears but no penguins, and the Antarctic has penguins but no polar bears. Let's talk about the Arctic first. The Arctic region consists of a vast, ice-covered ocean surrounded by treeless permafrost. The area can be defined as the region between the Arctic Circle and the North Pole. If you were to stand at the North Pole, everywhere you looked, in all directions, would be south. But standing at the North Pole is difficult to do for very long because it's in the middle of an ocean, covered by constantly shifting, frozen sea ice. If you were to fall into the water at the North Pole, you'd fall into water that's 13,980 feet deep. Above the water, average winter temperatures can be as low as -40 degrees Celsius, and the coldest recorded temperature is approximately -68 degrees Celsius. Despite these incredibly harsh conditions, humans have populated areas in the Arctic for thousands of years. Life in the Arctic includes organisms living in the ice, zooplankton and phytoplankton, fish and marine mammals, birds, land animals, plants, and human societies. Okay, what about Antarctica? Antarctica is Earth's southernmost continent, and it contains the geographic South Pole. It's the fifth largest continent on the planet at nearly twice the size of Australia. Almost 98% of Anarctica is covered by ice at least one mile in thickness. Conditions in Antarctica are some of the most extreme in the entire world. On average, it's the coldest, windiest, driest continent and has the highest average elevation of all the continents. You might think that it snows all the time at the Poles, but Antarctica is so dry, it's considered a desert with annual precipitation of only 200 millimeters along the coast and far less inland. The temperature in Antarctica has reached -89 degrees Celsius. Because it's so harsh and hard to get to, there are no permanent human residents on Antarctica, but anywhere from 1,000 to 5,000 people reside throughout the year at the research stations scattered across the continent. Even the most extreme animals fight for survival, and only cold-adapted organisms survive there, including many types of algae, animals, bacteria, fungi, plants, and protista. But why is Antarctica colder than its northern cousin? Well, first, much of the continent is more than three kilometers above sea level, and temperature decreases with elevation. That's why mountaintops have snow on them. Second, remember that the Arctic is really a frozen ocean. The water in the ocean beneath it is warmer than the frozen ground in the Antarctic, and that warmth is transferred through the ice pack. This prevents temperatures in the Arctic regions from reaching the extremes typical of the land surface of Antarctica. Third, the seasons are conspiring against the Antarctic. During the aphelion in July, when the Earth is the farthest away from the Sun, it also happens to be winter in the Antarctic, which creates a double-whammy of cold for the southern pole. But despite being inhospitable, the North and South Pole are a big reason why our planet is the way it is. Both of our polar regions are very important climate controllers. They help moderate the temperature in our temperate zones and give us stable weather. As sea ice in the Arctic declines due to climate change and global warming, weather around the globe becomes increasing more unstable.

See also

References

  1. ^ "Polar Deserts". Sand-boarding.com. 3 January 2022. Retrieved 11 August 2022.
  2. ^ Woodford, Chris (2011). Arctic Tundra and Polar Deserts. Chicago, Illinois: Heinemann-Raintree Books. pp. 6–7. ISBN 978-1-432-94172-7.
  3. ^ Priscu, John C.; et al. (1998). "Perennial Antarctic lake ice: an oasis for life in a polar desert". Science. 280 (5372): 2095–2098. Bibcode:1998Sci...280.2095P. doi:10.1126/science.280.5372.2095. JSTOR 2896532. PMID 9641910.

Public Domain This article incorporates public domain material from Types of Deserts. United States Geological Survey.


This page was last edited on 4 December 2023, at 18:46
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