Filchner Station

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Filchner Station
Antarctica relief location map.jpg
Red pog.svg
Filchner Station
Last location in Antarctica
Coordinates: 77°03′S50°03′W / 77.050°S 50.050°W / -77.050; -50.050
CountryFlag of Germany.svg  Germany
Location in Antarctica Filchner–Ronne Ice Shelf
Antarctica
Administered by Alfred Wegener Institute
EstablishedFebruary 1982 (1982-02)
SalvagedFebruary 1999 (1999-02)
Named for Wilhelm Filchner
TypeSummer
StatusClosed, lost
Website awi.de

Filchner Station was a German research station in the Antarctic. Administered by the Alfred Wegener Institute for Polar and Marine Research, it was established in February 1982 on the Filchner–Ronne Ice Shelf. The first station in Antarctica to be mounted on jacks, the structure was raised each year to allow for the increase in height of the shelf by snowfall. It was also relocated around 1 kilometre (0.62 mi) southwards each year to account for drift of the ice shelf. In October 1998, Filchner Station was stranded on iceberg A-38 when it broke away from the ice shelf. Research operations were cancelled and an emergency salvage operation was carried out that removed the majority of the station by February 1999.

Contents

Establishment and operation

The Filchner Station was established by the West German Alfred Wegener Institute for Polar and Marine Research (AWI) in February 1982. [1] [2] The station consisted of steel containers housing living quarters and laboratories. [3] The station was the first in the Antarctic to be mounted on jacks, allowing it to be raised in line with the increase in height of its surroundings due to snowfall. [4] The structure was typically jacked up by around 1 metre (3.3 ft) each year. [3] The structure could accommodate up to 26 personnel but was typically occupied only in the southern summer and by 12 people. [1] The station was sited approximately 20 kilometres (12 mi) from the edge of the Filchner–Ronne Ice Shelf which slowly drifts away from the continent. [1] To counteract this movement the station was moved around 1 kilometre (0.62 mi) southwards each of the 17 summers that it was staffed. [3] [4] It was maintained approximately at 77°03′S50°03′W / 77.050°S 50.050°W / -77.050; -50.050 . [3]

The station was resupplied by the AWI vessel Polarstern and also by Dornier aircraft which flew between the station, the German Neumayer Station II, the British Rothera Research Station and the Chilean Teniente R. Marsh Airport. [5] [6] The Filchner Station conducted studies on the mass of the ice shelf, geological and geophysical investigations in the Weddell Sea and meteorological work. Automatic instrumentation was installed to continue geophysical and meteorological investigations throughout the year, not just the summer period when the station was staffed. [1]

Loss

Iceberg A-38 calving from the Filchner-Ronne Ice Shelf Iceberg a-38.png
Iceberg A-38 calving from the Filchner–Ronne Ice Shelf

In October 1998 iceberg A-38 calved from the Filchner–Ronne Ice Shelf, the largest iceberg to do so for decades, carrying with it the Filchner Station. The station was to have been the main base for an 800 kilometres (500 mi) expedition in 1999; this was cancelled and replaced with an emergency salvage operation. The recovery of the base was a requirement of the environmental portions of the Antarctic Treaty. On 22 October A-38 split into two, Filchner remained on the western portion which became known as A-38B. [3]

The 10-man salvage team travelled on board Polarstern in early 1999 but became stranded in thick ice some 150 kilometres (93 mi) from the station. The ship was eventually freed and reached the 20 metres (66 ft) high edge of the iceberg in early February. Over the following 10 days some 120 tonnes (120 long tons) of the station were recovered as well as a further 50 tonnes (49 long tons) of vehicles. All that was left behind was the platform that the station was founded on. The loss of the station left the German research programme with only the Neumayer Station II in Antarctica. [3]

Related Research Articles

<span class="mw-page-title-main">Iceberg</span> Large piece of freshwater ice broken off a glacier or ice shelf and floating in open water

An iceberg is a piece of freshwater ice more than 15 m long that has broken off a glacier or an ice shelf and is floating freely in open (salt) water. Smaller chunks of floating glacially derived ice are called "growlers" or "bergy bits". Much of an iceberg is below the water's surface, which led to the expression "tip of the iceberg" to illustrate a small part of a larger unseen issue. Icebergs are considered a serious maritime hazard.

<span class="mw-page-title-main">Weddell Sea</span> Part of the Southern Ocean between Coats Land and the Antarctic Peninsula

The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha Coast, Queen Maud Land. To the east of Cape Norvegia is the King Haakon VII Sea. Much of the southern part of the sea is covered by a permanent, massive ice shelf field, the Filchner-Ronne Ice Shelf.

RV <i>Polarstern</i> German icebreaker and research vessel

RV Polarstern is a German research icebreaker of the Alfred Wegener Institute for Polar and Marine Research (AWI) in Bremerhaven, Germany. Polarstern was built by Howaldtswerke-Deutsche Werft in Kiel and Nobiskrug in Rendsburg, was commissioned in 1982, and is mainly used for research in the Arctic and Antarctica. The ship has a length of 118 metres and is a double-hulled icebreaker. She is operational at temperatures as low as −50 °C (−58 °F). Polarstern can break through ice 1.5 m thick at a speed of 5 knots. Thicker ice of up to 3 m (9.8 ft) can be broken by ramming.

<span class="mw-page-title-main">Ice shelf</span> Large floating platform of ice caused by glacier flowing onto ocean surface

An ice shelf is a large floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface. Ice shelves are found in Antarctica and the Arctic. The boundary between the floating ice shelf and the anchor ice that feeds it is the grounding line. The thickness of ice shelves can range from about 100 m (330 ft) to 1,000 m (3,300 ft). The world's largest ice shelves are the Ross Ice Shelf and the Filchner-Ronne Ice Shelf in Antarctica. When a large piece of an ice shelf breaks off, this can lead to the formation of an iceberg. This process is also called ice calving.

<span class="mw-page-title-main">Filchner–Ronne Ice Shelf</span> Ice shelf in Antarctica

The Filchner–Ronne Ice Shelf or Ronne–Filchner Ice Shelf is an Antarctic ice shelf bordering the Weddell Sea.

<span class="mw-page-title-main">Berkner Island</span> Ice rise in the British Antarctic Territory, Antarctica

Berkner Island is an Antarctic ice rise, where bedrock below sea level has caused the surrounding ice sheet to create a dome. If the ice cap were removed, the island would be underwater. Berkner Island is completely ice-covered and is about 320 kilometres (200 mi) long and 150 kilometres (93 mi) wide, with an area of 44,000 km2 (17,000 sq mi). It is surrounded by the Filchner-Ronne Ice Shelf. The northernmost point of the Berkner is about 20 kilometres (12 mi) from the open sea. It lies in the overlapping portion of the Argentine and the British Antarctic territorial claims.

<span class="mw-page-title-main">Alfred Wegener Institute for Polar and Marine Research</span>

The Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research is located in Bremerhaven, Germany, and a member of the Helmholtz Association of German Research Centres. It conducts research in the Arctic, the Antarctic, and the high and mid latitude oceans. Additional research topics are: North Sea research, marine biological monitoring, and technical marine developments. The institute was founded in 1980 and is named after meteorologist, climatologist, and geologist Alfred Wegener.

<span class="mw-page-title-main">Amery Ice Shelf</span> Ice shelf in Antarctica

The Amery Ice Shelf is a broad ice shelf in Antarctica at the head of Prydz Bay between the Lars Christensen Coast and Ingrid Christensen Coast. It is part of Mac. Robertson Land. The name "Cape Amery" was applied to a coastal angle mapped on 11 February 1931 by the British Australian New Zealand Antarctic Research Expedition (BANZARE) under Douglas Mawson. He named it for William Bankes Amery, a civil servant who represented the United Kingdom government in Australia (1925–28). The Advisory Committee on Antarctic Names interpreted this feature to be a portion of an ice shelf and, in 1947, applied the name Amery to the whole shelf.

<span class="mw-page-title-main">Luitpold Coast</span> Coastal region of Antarctica

Luitpold Coast is that portion of the coast of Coats Land extending from the vicinity of Hayes Glacier, at 27°54′W, to 36°W, which is regarded as the eastern limit of the Filchner Ice Shelf. It was discovered by Wilhelm Filchner, leader of the Second German Antarctic Expedition, 1911–12, and named after Luitpold, Prince Regent of Bavaria.

<span class="mw-page-title-main">Second German Antarctic Expedition</span> Antarctic research expedition

The Second German Antarctic Expedition of 1911–1913 was led by Wilhelm Filchner in the exploration ship Deutschland. Its principal objective was to determine whether the Antarctic continent comprised a single landmass rather than separated elements, and in particular whether the Weddell Sea and Ross Sea were connected by a strait. In addition, an extensive programme of scientific research was undertaken. The expedition failed to establish a land base, and the ship became beset in the Weddell Sea ice, drifting north for eight months before reaching open water. The expedition was marred by considerable disagreement and animosity among its participants, and broke up in disarray.

<span class="mw-page-title-main">Neumayer Station III</span> Antarctic base

Neumayer Station III, also known as Neumayer III after geophysicist Georg von Neumayer, is a German Antarctic research station of the Alfred-Wegener-Institut. It is located on the approximately 200 metres (660 ft) thick Ekström Ice Shelf several kilometres south of Neumayer Station II. The station's assembly kit was transported to its current position early in November 2007. It is moving with the shelf ice at about 157 meters (515 ft) per year towards the open sea.

<span class="mw-page-title-main">Ellsworth Station</span> Antarctic base in Tierra del Fuego

Ellsworth Scientific Station was a permanent, all year-round originally American, then Argentine Antarctic scientific research station named after American polar explorer Lincoln Ellsworth. It was located on Gould Bay, on the Filchner Ice Shelf.

<span class="mw-page-title-main">Kohnen Station</span> Antarctic base

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<span class="mw-page-title-main">Ice2sea</span>

Ice2sea was a program of scientific research funded by the European Union's Framework 7 Programme to study the effects of climate change on glaciation and the melting of ice caps and glaciers on sea level. The ice2sea project, a collaborative of 24 research institutions, which was headed by Prof David Vaughan, aimed to reduce the uncertainty in sea-level projections which are of great economic and social importance to European, especially as large areas of coastal Europe are below or less than a metre above sea level.

<span class="mw-page-title-main">Iceberg A-38</span> Large iceberg that split from the Filchner-Ronne Ice Shelf in Antarctica in 1998

A-38 was a large iceberg that split from the Filchner-Ronne Ice Shelf in Antarctica in October 1998. Soon after formation it split into two pieces, A-38A and A-38B, which drifted westwards on the Weddell Gyre. The icebergs moved north along the Antarctic Peninsula and reached its tip in February 2003. A-38A and A-38B increased speed in open sea and grounded in shallower waters to the east of South Georgia Island in December 2003. A-38A broke up into three pieces in March 2004 and drifted north where it decayed. A-38B split into two in April, with the eastern portion, now known as A-38G, drifting north and west to decay. The remainder of A-38B remained grounded, interfering with the foraging routes of seals and penguins in South Georgia, resulting in the deaths of their young. On 20 August A38-B broke into two, with the new portion drifting north and breaking up. The remainder of A-38B continued to break up through September 2004 and had completely decayed by 2005.

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References

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  2. Meeresforschung, Alfred-Wegener-Institut für Polar- und (1998). Report. The Institute. p. 14.
  3. 1 2 3 4 5 6 Heuseler, Holger (1 July 1999). "Zerrissene Hoffnungen". Wissenschaft (in German). Retrieved 5 November 2020.
  4. 1 2 Zufelt, Jon E. (1999). Cold Regions Engineering: Putting Research Into Practice : Proceedings of the Tenth International Conference, August 16–19, 1999, Lincoln, New Hampshire. American Society of Civil Engineers. p. 79. ISBN   978-0-7844-0451-5.
  5. Antarctic. New Zealand Antarctic Society. 1986. p. 209.
  6. Antarctic. New Zealand Antarctic Society. 1986. p. 168.