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| Antarctica (continent) | |
|---|---|
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| Name | Antarctica |
| Caption | Satellite composite of Antarctica |
| Area km2 | 14000000 |
| Population | 0 (permanent) |
| Highest point | Mount Vinson |
| Highest elevation m | 4892 |
| Languages | None (no indigenous population) |
| Coordinates | 82°S 135°E |
Antarctica (continent) is Earth's southernmost continent, centered on the South Pole and almost entirely south of the Antarctic Circle. It is the coldest, windiest, and driest continental landmass, dominated by the Antarctic Ice Sheet and surrounded by the Southern Ocean. The continent has no indigenous human population and is governed under a unique international framework emphasizing scientific cooperation and environmental protection.
The name "Antarctica" derives from the Greek ἀνταρκτικός (antarktikós), meaning "opposite the Arctic", a term used by ancient Greek geographers and later adopted in modern cartography and exploration narratives. Early uses appear in the works of Claudius Ptolemy and later mapmakers; the concept of a southern landmass influenced expeditions like those led by James Cook and theories discussed at gatherings such as the Age of Discovery. Formal naming was consolidated during the era of polar voyages by figures including Fabian Gottlieb von Bellingshausen, James Clark Ross, and explorers affiliated with organizations like the Royal Geographical Society.
Antarctica is roughly triangular in plan and divided by the Transantarctic Mountains into East Antarctica (Antarctic Plateau) and West Antarctica (including the Antarctic Peninsula). Major topographic features include Mount Vinson in the Sentinel Range, the Transantarctic Mountains, and subglacial Lake Vostok. The continental crust and tectonic history record interactions with ancient supercontinents such as Gondwana; rock exposures in regions like the McMurdo Dry Valleys preserve records studied by geologists from institutions including the Scott Polar Research Institute and the United States Geological Survey. Surrounding seas—Weddell Sea, Ross Sea, and Amundsen Sea—connect to the Southern Ocean, with bathymetry shaping ice-shelf formation and marine currents tied to global systems studied by programs like the International Geophysical Year.
The Antarctic climate is characterized by frigid polar conditions, katabatic winds, and polar deserts; temperature and precipitation patterns vary between the high interior plateau and coastal margins. The Antarctic Ice Sheet, comprising the East Antarctic Ice Sheet and West Antarctic Ice Sheet, contains the vast majority of Earth's freshwater and influences global sea level — a focus of research by the Intergovernmental Panel on Climate Change, National Aeronautics and Space Administration, and European Space Agency. Ice shelves such as the Ross Ice Shelf and Filchner–Ronne Ice Shelf buttress outlet glaciers; processes like ice-shelf collapse (e.g., events affecting Larsen Ice Shelf) and grounding-line retreat are documented in studies by British Antarctic Survey, Scripps Institution of Oceanography, and the Alfred Wegener Institute. Paleoclimate records from ice cores at Dome C, Dome Fuji, and Byrd Station provide proxies used in reconstructing past atmospheric composition and climate events including glacial-interglacial cycles.
Terrestrial life is sparse and specialized: cryptogamic communities, mosses, lichens, and microbial mats inhabit ice-free oases such as the McMurdo Dry Valleys and subantarctic islands. The surrounding Southern Ocean supports rich marine ecosystems with keystone species including Antarctic krill, which sustain populations of Adélie penguin, Emperor penguin, Weddell seal, leopard seal, and migratory cetaceans like the Southern right whale and Orca. Seabird distributions feature species such as the albatross and Antarctic petrel. Biodiversity research is conducted by institutes including the Australian Antarctic Division, Instituto Antártico Argentino, and the Polar Research Institute of China, often in association with conservation frameworks under treaties like the Convention on the Conservation of Antarctic Marine Living Resources.
Human interaction began with nineteenth- and twentieth-century exploration by expeditions led by Ernest Shackleton, Roald Amundsen, Robert Falcon Scott, Douglas Mawson, and Richard E. Byrd. Key events include the attainment of the South Pole by Amundsen and the tragic Terra Nova Expedition led by Scott. The early twentieth-century "Heroic Age of Antarctic Exploration" attracted national programs from United Kingdom, Norway, United States, Australia, France, and Argentina. Aviation and mechanized logistics advanced during mid-century campaigns associated with the Operation Highjump and scientific initiatives such as the International Geophysical Year (1957–58), which expanded permanent stations like McMurdo Station and Mawson Station.
Antarctica is regulated by the Antarctic Treaty system, originating with the 1959 Antarctic Treaty and expanded through measures and agreements including the Protocol on Environmental Protection to the Antarctic Treaty (Madrid Protocol) and the Convention for the Conservation of Antarctic Seals. The treaty designates Antarctica as a scientific preserve, suspends territorial sovereignty claims by parties including United Kingdom, Chile, Argentina, Australia, New Zealand, France, and Norway, and prohibits military activity and mineral resource exploitation under current protocols. Governance structures feature consultative meetings with participation by signatory states such as Russia, China, United States, Germany, and South Africa.
Antarctica hosts a global network of research stations operated by national programs like the British Antarctic Survey, United States Antarctic Program, Australian Antarctic Division, Instituto Antártico Chileno, and Vostok Station-related efforts. Scientific disciplines include glaciology, paleoclimatology, astrophysics (e.g., facilities at South Pole Station for cosmic microwave background studies), oceanography, and ecology. Major multinational projects include the Antarctic Treaty Consultative Meeting-endorsed initiatives, ice-core campaigns at Dome C (by European Project for Ice Coring in Antarctica), and collaborative logistics coordinated via Scientific Committee on Antarctic Research. Long-term monitoring addresses climate change impacts, sea-level projections by the Intergovernmental Panel on Climate Change, and conservation measures under the Commission for the Conservation of Antarctic Marine Living Resources.
Category:Continents