Observations beneath Pine Island Glacier in West Antarctica and implications for its retreat
Jenkins, Adrian; Dutrieux, Pierre; Jacobs, Stanley. S.; McPhail, Stephen. D.; Perrett, James. R.; Webb, Andrew. T.; White, David. 2010 Observations beneath Pine Island Glacier in West Antarctica and implications for its retreat. Nature Geoscience, 3 (7). 468-472. 10.1038/ngeo890Full text not available from this repository.
Thinning ice in West Antarctica, resulting from acceleration in the flow of outlet glaciers, is at present contributing about 10% of the observed rise in global sea level1. Pine Island Glacier in particular has shown nearly continuous acceleration2, 3 and thinning4, 5, throughout the short observational record. The floating ice shelf that forms where the glacier reaches the coast has been thinning rapidly6, driven by changes in ocean heat transport beneath it. As a result, the line that separates grounded and floating ice has retreated inland7. These events have been postulated as the cause for the inland thinning and acceleration8, 9. Here we report evidence gathered by an autonomous underwater vehicle operating beneath the ice shelf that Pine Island Glacier was recently grounded on a transverse ridge in the sea floor. Warm sea water now flows through a widening gap above the submarine ridge, rapidly melting the thick ice of the newly formed upstream half of the ice shelf. The present evolution of Pine Island Glacier is thus part of a longer-term trend that has moved the downstream limit of grounded ice inland by 30 km, into water that is 300 m deeper than over the ridge crest. The pace and ultimate extent of such potentially unstable retreat10 are central to the debate over the possibility of widespread ice-sheet collapse triggered by climate change
|Programmes:||BAS Programmes > Polar Science for Planet Earth (2009 - ) > Polar Oceans|
|NORA Subject Terms:||Marine Sciences
Meteorology and Climatology
|Date made live:||27 Jul 2010 15:36|
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