The
Larsen Ice Shelf is a long, fringing
ice shelf in the northwest part of the
Weddell Sea, extending along the east coast of
Antarctic Peninsula from
Cape Longing to the area just southward of
Hearst Island. Named for Captain
Carl Anton Larsen, the master of the Norwegian whaling vessel
Jason, who sailed along the ice front as far as 68°10' South during December 1893.
In finer detail, the Larsen Ice Shelf is a series of three shelves that occupy (or occupied) distinct embayments along the coast. From north to south, the three segments are called Larsen A (the smallest), Larsen B, and Larsen C (the largest) by researchers who work in the area. The Larsen A ice shelf disintegrated in January 1995. The Larsen B ice shelf disintegrated in February 2002. The Larsen C ice shelf appears to be stable for the time being, though scientists predict that, if localized warming continues at its current rate, the shelf could disintegrate at some point within the foreseeable future.
The Larsen disintegration events were unusual by past standards. Typically, ice shelves lose mass by
iceberg calving and by melting at their upper and lower surfaces. The disintegration events are linked to the ongoing
climate warming in the
Antarctic Peninsula, about 0.5 °C per decade since the late 1940s, which is a consequence of localized warming of the Antarctic peninsula.Connor, Steve (2005) "Ice shelf collapse was biggest...
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