2015 in Antarctica

Last updated
Proposed flag of Antarctica (Graham Bartram).svg
2015
in
Antarctica
Decades:
See also:

The following is a list of events that occurred in Antarctica in 2015 .

Events

Related Research Articles

<span class="mw-page-title-main">Meteorite</span> Solid debris from outer space that hits a planetary surface

A meteorite is a solid piece of debris from an object, such as a comet, asteroid, or meteoroid, that originates in outer space and survives its passage through the atmosphere to reach the surface of a planet or moon. When the original object enters the atmosphere, various factors such as friction, pressure, and chemical interactions with the atmospheric gases cause it to heat up and radiate energy. It then becomes a meteor and forms a fireball, also known as a shooting star; astronomers call the brightest examples "bolides". Once it settles on the larger body's surface, the meteor becomes a meteorite. Meteorites vary greatly in size. For geologists, a bolide is a meteorite large enough to create an impact crater.

<span class="mw-page-title-main">Peter I Island</span> Island in Antarctica

Peter I Island is an uninhabited volcanic island in the Bellingshausen Sea, 450 kilometres (240 nmi) from continental Antarctica. It is claimed as a dependency of Norway and, along with Bouvet Island and Queen Maud Land, composes one of the three Norwegian dependent territories in the Antarctic and Subantarctic. The island measures approximately 11 by 19 kilometres, with an area of 156 km2 (60 sq mi); its highest point is the ultra-prominent, 1,640-metre-tall (5,380 ft) Lars Christensen Peak. Nearly all the island is covered by a glacier, and it is surrounded most of the year by pack ice, making it inaccessible during these times. There is little vertebrate animal life on the island, apart from some seabirds and seals.

<span class="mw-page-title-main">Lunar meteorite</span> Meteorite that originated from the Moon

A lunar meteorite is a meteorite that is known to have originated on the Moon. A meteorite hitting the Moon is normally classified as a transient lunar phenomenon.

<span class="mw-page-title-main">New Swabia</span> A territory of Antarctica in Queen Maud Land, first explored by Nazi Germany in 1938/39

New Swabia was a disputed Antarctic claim by Nazi Germany within the Norwegian territorial claim of Queen Maud Land and is now a cartographic name sometimes given to an area of Antarctica between 20°E and 10°W in Queen Maud Land. New Swabia was explored by Germany in early 1939 and named after that expedition's ship, Schwabenland, itself named after the German region of Swabia.

<span class="mw-page-title-main">Coats Land</span> Geographic region

Coats Land is a region in Antarctica which lies westward of Queen Maud Land and forms the eastern shore of the Weddell Sea, extending in a general northeast–southwest direction between 20°00′W and 36°00′W. The northeast part was discovered from the Scotia by William S. Bruce, leader of the Scottish National Antarctic Expedition, 1902-1904. He gave the name Coats Land for James Coats, Jr., and Major Andrew Coats, the two chief supporters of the expedition.

Wilkes Land crater is an informal term that may apply to two separate cases of conjectured giant impact craters hidden beneath the ice cap of Wilkes Land, East Antarctica. These are separated below under the heading Wilkes Land anomaly and Wilkes Land mascon (mass concentration), based on terms used in their principal published reference sources.

<span class="mw-page-title-main">Troll Airfield</span> Airstrip in Queen Maud Land, Antarctica

Troll Airfield is an airstrip located 6.8 kilometres (4.2 mi) from the research station Troll in Princess Martha Coast in Queen Maud Land, Antarctica. Owned and operated by the Norwegian Polar Institute, it consists of a 3,300-by-100-metre runway on glacial blue ice on the Antarctic ice sheet. The airport is located at 1,232 metres (4,042 ft) above mean sea level and is 235 kilometres (146 mi) from the coast.

Adelie Land is a meteorite discovered on December 5, 1912, in Antarctica by Francis Howard Bickerton (1889-1954), a member of Sir Douglas Mawson's Australasian Antarctic Expedition. It was named after Adélie Land and it was the first meteorite found in Antarctica.

<span class="mw-page-title-main">National Institute of Polar Research (Japan)</span>

National Institute of Polar Research, NIPR is the research institute responsible for scientific research and observation of the polar regions. NIPR manages several observation stations in the Arctic and Antarctica. It was founded in 1973.

<span class="mw-page-title-main">Territorial claims in Antarctica</span> Land claims of the continent

Seven sovereign states – Argentina, Australia, Chile, France, New Zealand, Norway, and the United Kingdom – have made eight territorial claims in Antarctica. These countries have tended to place their Antarctic scientific observation and study facilities within their respective claimed territories; however, a number of such facilities are located outside of the area claimed by their respective countries of operation, and countries without claims such as China, India, Italy, Japan, Pakistan, Russia, South Africa (SANAE), Poland, and the United States have constructed research facilities within the areas claimed by other countries. There are overlaps among the territories claimed by Argentina, Chile, and the United Kingdom.

<span class="mw-page-title-main">Antarctica</span> Continent

Antarctica is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of 14,200,000 km2 (5,500,000 sq mi). Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of 1.9 km (1.2 mi).

<span class="mw-page-title-main">Queen Maud Land</span> Norways territorial claim in Antarctica

Queen Maud Land is a roughly 2.7-million-square-kilometre (1.0-million-square-mile) region of Antarctica claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20° west and the Australian Antarctic Territory 45° east. In addition, a small unclaimed area from 1939 was annexed in June 2015. Positioned in East Antarctica, it makes out about one-fifth of the continent, and is named after the Norwegian Queen Maud (1869–1938).

<span class="mw-page-title-main">Dependencies of Norway</span> Territories of Norway in the Southern Hemisphere

Norway has three dependent territories, all uninhabited and located in the Southern Hemisphere. Bouvet Island (Bouvetøya) is a sub-Antarctic island in the South Atlantic Ocean. Queen Maud Land is the sector of Antarctica between the 20th meridian west and the 45th meridian east. Peter I Island is a volcanic island located 450 kilometres (280 mi) off the coast of Ellsworth Land of continental Antarctica. Despite being unincorporated areas, neither Svalbard nor Jan Mayen is formally considered a dependency. While the Svalbard Treaty regulates some aspects of that Arctic territory, it acknowledges that the islands are part of Norway. Similarly, Jan Mayen is recognized as an integral part of Norway.

The sixth Norwegian Antarctic Expedition was a scientific expedition to Queen Maud's Land in Antarctica. The expedition was based at Norway Station which was located on the Fimbul Ice Shelf bordering the coast of Queen Maud Land.

<span class="mw-page-title-main">Nakhlite</span> Group of Martian meteorites

Nakhlites are a group of Martian meteorites, named after the first one, Nakhla meteorite.

<span class="mw-page-title-main">King Baudouin Ice Shelf</span>

The King Baudouin Ice Shelf in Dronning Maud Land, East Antarctica, is within the Norwegian part of Antarctica. It is named after King Baudouin of Belgium (1930-1993).

<span class="mw-page-title-main">Blue-ice area</span> Blue area of an ice sheet

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 by topographic obstacles such as mountains that emerge from the ice sheet, generating particular climatic conditions where the net snow accumulation is exceeded by wind-driven sublimation and snow transports.

References

  1. "Sudden Impact: Did Meteorite Carve Icy Crater in Antarctica?". NBC News. Retrieved 6 May 2018.
  2. "Norge utvider Dronning Maud Land helt frem til Sydpolen". Aftenposten (in Norwegian Bokmål). Retrieved 6 May 2018.
  3. "Minnesota woman conquered Antarctica marathon. Now she's raced at the North Pole". Star Tribune. Retrieved 6 May 2018.