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  2. West Antarctic Ice Sheet - Wikipedia

    en.wikipedia.org/wiki/West_Antarctic_Ice_Sheet

    A map of West Antarctica. The total volume of the entire Antarctic ice sheet is estimated at 26.92 million km 3 (6.46 million cu mi), [2] while the WAIS contains about 2.1 million km 3 (530,000 cu mi) in ice that is above the sea level, and ~1 million km 3 (240,000 cu mi) in ice that is below it. [20]

  3. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    Because the East Antarctic ice sheet is over 10 times larger than the West Antarctic ice sheet and located at a higher elevation, it is less vulnerable to climate change than the WAIS. In the 20th century, EAIS had been one of the only places on Earth which displayed limited cooling instead of warming, even as the WAIS warmed by over 0.1 °C ...

  4. West Antarctica - Wikipedia

    en.wikipedia.org/wiki/West_Antarctica

    Geographical map of Antarctica. Lying on the Pacific Ocean side of the Transantarctic Mountains, West Antarctica comprises the Antarctic Peninsula (with Graham Land and Palmer Land) and Ellsworth Land, Marie Byrd Land and King Edward VII Land, offshore islands such as Adelaide Island, and ice shelves, notably the Filchner-Ronne Ice Shelf on the Weddell Sea, and the Ross Ice Shelf on the Ross Sea.

  5. WAIS Divide - Wikipedia

    en.wikipedia.org/wiki/WAIS_Divide

    The WAIS Divide is the ice flow divide on the West Antarctic Ice Sheet (WAIS) which is a linear boundary that separates the region where the ice flows to the Ross Sea, from the region where the ice flows to the Weddell Sea. It is similar to a continental hydrographic divide.

  6. Doomsday Glacier won’t collapse in coming decades, but ...

    www.aol.com/doomsday-glacier-won-t-collapse...

    A minuscule part of the West Antarctic ice sheet, the glacier is located 7,000 miles to the south of the western US. The widest glacier on Earth, it spans across 74,000 miles and extends thousands ...

  7. John H. Mercer - Wikipedia

    en.wikipedia.org/wiki/John_H._Mercer

    If contact of ice to bottom rocks is lost seaward of the grounding line, the ice sheet becomes significantly thinner (some 100 m), forming a shelf ice. John H. Mercer (19 October 1922 – 3 July 1987) was a British glaciologist, chiefly known for his theoretical work on, and field studies of Antarctic ice streams , especially in the ...

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