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  2. Antarctic Circumpolar Current - Wikipedia

    en.wikipedia.org/wiki/Antarctic_Circumpolar_Current

    The current is circumpolar due to the lack of any landmass connecting with Antarctica and this keeps warm ocean waters away from Antarctica, enabling that continent to maintain its huge ice sheet. Associated with the Circumpolar Current is the Antarctic Convergence , where the cold Antarctic waters meet the warmer waters of the subantarctic ...

  3. Blue-ice area - Wikipedia

    en.wikipedia.org/wiki/Blue-ice_area

    A blue-ice area is an ice-covered area of Antarctica where wind-driven snow transport and sublimation result in net mass loss from the ice surface in the absence of melting, forming a blue surface that contrasts with the more common white Antarctic surface. Such blue-ice areas typically form when the movement of both air and ice are obstructed ...

  4. Katabatic wind - Wikipedia

    en.wikipedia.org/wiki/Katabatic_wind

    Coastal polynyas are produced in the Antarctic by katabatic winds. Katabatic winds are for example found blowing out from the large and elevated ice sheets of Antarctica and Greenland. The buildup of high density cold air over the ice sheets and the elevation of the ice sheets brings into play enormous gravitational energy.

  5. Record low sea-ice levels around Antarctica ‘likely due to ...

    www.aol.com/record-low-sea-ice-levels-130000999.html

    Antarctica’s vast expanse of sea ice regulates Earth’s temperature, as the white surface reflects the Sun’s heat back into the atmosphere. Record low sea-ice levels around Antarctica ...

  6. Southern Ocean overturning circulation - Wikipedia

    en.wikipedia.org/wiki/Southern_Ocean_overturning...

    A schematic overview of the Southern Ocean overturning circulation. The arrows point in the direction of the water movement. The lower cell of the circulation is depicted by the upwelling arrows south of the Antarctic Circumpolar Current (ACC) and the formation of Antarctic Bottom Water beneath the sea ice of Antarctica due to buoyancy loss.

  7. Antarctic Cold Reversal - Wikipedia

    en.wikipedia.org/wiki/Antarctic_Cold_Reversal

    Record of atmospheric temperature taken from EPICA ice core in Antarctica. The Antarctic Cold Reversal (ACR) was a climatic event of intense atmospheric and oceanic cooling across the southern hemisphere (>40°S) between 14,700 and 13,000 years before present that interrupted the most recent deglacial climate warming (c. 18,000-11,500 years BP).

  8. Climate change in Antarctica - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_Antarctica

    Antarctic surface ice layer temperature trends between 1981 and 2007, based on thermal infrared observations made by a series of NOAA satellite sensors.. 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, [1] climate change in Antarctica has been observed.

  9. Climate of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Climate_of_Antarctica

    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 km 3 (7.2 × 10 ^ 6 cu mi) of ice — the seas would rise by over 60 m (200 ft ...