رصيف لارسن الجليدي

Coordinates: 67°30′S 62°30′W / 67.500°S 62.500°W / -67.500; -62.500
Larsen Ice Shelves A, B, C, and D
Location of the Antarctic Peninsula within Antarctica

رصيف لارسن الجليدي Larsen Ice Shelf هو رصيف جليدي طويل في الجزء الشمالي الغربي من بحر ودل، ويمتد بطول الساحل الشرقي لـشبه جزيرة أنتارتيكا من رأس لونگنگ إلى المنطقة إلى الجنوب مباشرة من جزيرة هيرست. وهو مسمى على اسم الكاپتن كارل أنطون لارسن، سيد سفينة صيد الحيتان النرويجية Jason, who sailed along the ice front as far as 68°10' South during December 1893.[1] In finer detail, the Larsen Ice Shelf is a series of shelves that occupy (or occupied) distinct embayments along the coast. From north to south, the segments are called Larsen A (the smallest), Larsen B, and Larsen C (the largest) by researchers who work in the area.[2] Further south, Larsen D and the much smaller Larsen E, F and G are also named.[3][4]

The breakup of the ice shelf since the mid-1990s has been widely reported,[5] with the collapse of Larsen B in 2002 being particularly dramatic. A large section of the Larsen C shelf was reported to have broken away in the week beginning 10 July 2017.[6]

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الرصيف الجليدي

Processes around an Antarctic ice shelf


الانفصال

An image of the collapsing Larsen B Ice Shelf and a comparison of this to the U.S. state of Rhode Island.

لارسن A

The Larsen A ice shelf disintegrated in January 1995.[2]

لارسن B

The collapse of Larsen B, showing the diminishing extent of the shelf from 1998 to 2002.

From 31 January 2002 to March 2002 the Larsen B sector partially collapsed and parts broke up, 3,250 km2 (1,250 sq mi) of ice 220 m (720 ft) thick, an area comparable to the US state of Rhode Island.[7] In 2015, a study concluded that the remaining Larsen B ice-shelf will disintegrate by 2020, based on observations of faster flow and rapid thinning of glaciers in the area.[8]

لارسن C

2016 rift in Larsen C, wide view
Four figures showing 1) how the buoyancy of an ice shelf supports the descending glacier, slowing its motion, 2) how warmer temperatures reduce the mass of the ice shelf and provide more meltwater to lubricate the glacier, causing it to move faster, 3) how a missing ice shelf leads to more rapid glacier motion and rapid calving into the sea, and 4) how this leads to a thinner glacier with a steeper surface which moves even faster
Glacier–ice shelf interactions.
Updated graphic of 1 May 2017, showing new fracture branching off existing crack, with new fracture heading towards ice shelf just 19 km (12 mi) away. Graphic from PROJECT MIDAS, A. Luckman, Swansea University

اعتبارا من July 2017, Larsen C is the fourth largest ice shelf in Antarctica, with an area of about 44,200 km2 (17,100 sq mi).[9]

لارسن D

The Larsen D Ice Shelf is located between Smith Peninsula in the south and Gipps Ice Rise in the north. It is considered to be generally stable. Over roughly the past fifty years it has advanced where the other ice shelves George VI, Bach, Stange, and Larsen C have all retreated. However, this gain has been relatively small in comparison to the retreat of the others. The most recent survey of Larsen D measured it at 22,600 square kilometres. There is fast ice along the entire front. This makes it difficult to interpret the ice front because the semi-permanent sea ice varies in thickness and may be nearly indistinguishable from shelf ice.[10]

معرض صور

  • Larsen A and Larsen B ice shelves marked in red.

    Larsen A and Larsen B ice shelves marked in red.

  • Clear view of the Antarctic Peninsula, the Larsen Ice Shelf, and the sea ice covered waters around the region.

    Clear view of the Antarctic Peninsula, the Larsen Ice Shelf, and the sea ice covered waters around the region.

  • Larsen B area in March 2013

    Larsen B area in March 2013

  • 2016 rift in Larsen C, detail

    2016 rift in Larsen C, detail

انظر أيضاً

الهامش

  1. ^ U.S. Geological Survey Geographic Names Information System: رصيف لارسن الجليدي
  2. ^ أ ب Fox, Douglas. "Witness to an Antarctic Meltdown". 307 (1): 54–61. doi:10.1038/scientificamerican0712-54. {{cite journal}}: Cite journal requires |journal= (help)
  3. ^ Rignot, E; Jacobs, S; Mouginot, J; Scheuchl, B (13 June 2013). "Ice Shelf Melting Around Antarctica" (PDF). Science. 341 (6143): 266–270. doi:10.1126/science.1235798. Retrieved 21 January 2017.
  4. ^ ice Break in Antartica
  5. ^ Chris Wickham (9 May 2012). "Warm water threatens vast Antarctic ice shelf (+video)". The Christian Science Monitor / Reuters. Retrieved 20 January 2017.
  6. ^ "Iceberg four times the size of London breaks off from Antarctica ice shelf". The Daily Telegraph. 12 July 2017.
  7. ^ Hulbe, Christina (2002). "Larsen Ice Shelf 2002, warmest summer on record leads to disintegration". Portland State University.
  8. ^ "NASA Study Shows Antarctica's Larsen B Ice Shelf Nearing Its Final Act" (Press release). NASA. 14 May 2015.
  9. ^ "Growing Crack in Antarctica's Larsen C Ice Shelf Spotted by NASA's MISR".
  10. ^ Overview of areal changes of the ice shelves on the Antarctic Peninsula over the past 50 years. The Cryosphere Discussions. 3 pp579-630. URL: http://www.the-cryosphere-discuss.net/3/579/2009/tcd-3-579-2009.pdf

وصلات خارجية

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خطأ لوا في وحدة:Authority_control على السطر 278: attempt to call field '_showMessage' (a nil value). 67°30′S 62°30′W / 67.500°S 62.500°W / -67.500; -62.500

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