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Andrew Shepherd,1*Duncan Wingham,2Tony Payne,3Pedro Skvarca4
The retreat and collapse of Antarctic Peninsula ice shelvesin tandem with a regional atmospheric warming has fueled speculationas to how these events may be related. Satellite radar altimetermeasurements show that between 1992 and 2001 the Larsen IceShelf lowered by up to 0.27 ± 0.11 meters per year. Thelowering is explained by increased summer melt-water and theloss of basal ice through melting. Enhanced ocean-driven meltingmay provide a simple link between regional climate warming andthe successive disintegration of sections of the Larsen IceShelf.
1 Centre for Polar Observation and Modelling, Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK. 2 Centre for Polar Observation and Modelling, University College London, Gower Street, London WC1E 6BT, UK. 3 Centre for Polar Observation and Modelling, University of Bristol, University Road, Bristol BS8 1SS, UK. 4 Instituto Antártico Argentino, Cerrito 1248, 1010 Buenos Aires, Argentina.
* To whom correspondence should be addressed. E-mail: aps46{at}cam.ac.uk