West Antarctica is largely covered by the Antarctic ice sheet, but there have been signs that climate change is having some effect and that this ice sheet may have started to shrink slightly. Over the past 50 years, the west coast of the Antarctic Peninsula has been – and still is – one of the most rapidly warming parts of the planet,[1][2] and the coasts of the Peninsula are the only parts of West Antarctica that become (in summer) ice-free. These constitute the Marielandia Antarctic tundra and have the warmest climate in Antarctica. The rocks are clad in mosses and lichens that can cope with the intense cold of winter and the short growing-season.
West Antarctica was named in the early 20th century.[3] That usage became standard following the International Geophysical Year (1957–1958) and explorations which disclosed that the Transantarctic Mountains provide a useful regional border between West Antarctica and East Antarctica. The Advisory Committee on Antarctic Names approved the name in 1962.
West Antarctica is mostly covered by a massive ice sheet referred to as the West Antarctic Ice Sheet. In recent decades, this ice sheet has shown signs of decreasing mass.[4]
The geologic history of West Antarctica was summarized in a 2020 publication.[5]
Marielandia Antarctic tundra
The parts of West Antarctica not covered with ice (Antarctic oasis), which are the coasts of the Antarctic Peninsula, constitute a biodiversity region known as Marielandia Antarctic tundra (after Marie Byrd Land).[6] This area has the warmest climate in Antarctica and the moss and lichen-covered rocks are free of snow during the summer months, although the weather is still intensely cold and the growing season very short.
^Jordan, Tom A.; Riley, Teal R.; Siddoway, Christine S. (2020). "The geological history and evolution of West Antarctica". Nature Reviews Earth & Environment. 1 (2): 117–133. doi:10.1038/s43017-019-0013-6. ISSN2662-138X.
^World Wildlife Fund, ed. (2001). "Marielandia Antarctic tundra". WildWorld Ecoregion Profile. National Geographic Society. Archived from the original on 2010-03-08. Retrieved 2008-01-26.