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Gladstone, Rupert M.; Lee, Victoria; Rougier, Jonathan; Payne, Antony J.; Hellmer, Hartmut; Le Brocq, Anne; Shepherd, Andrew; Edwards, Tamsin L.; Gregory, Jonathan and Cornford, Stephen L.
(2012).
DOI: https://doi.org/10.1016/j.epsl.2012.04.022
Abstract
A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B ‘business as usual’ emissions scenario. Comparison is made against recent observations to provide a calibrated prediction in the form of a 95% confidence set. Predictions are for monotonic (apart from some small scale fluctuations in a minority of cases) retreat of the grounding line over the next 200 yr with huge uncertainty in the rate of retreat. Full collapse of the main trunk of the PIG during the 22nd century remains a possibility.
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About
- Item ORO ID
- 48983
- Item Type
- Journal Item
- ISSN
- 0012-821X
- Project Funding Details
-
Funded Project Name Project ID Funding Body ice2sea programme Not Set European Union FP7 Understanding contemporary change in the West Antarctic ice sheet NE/E006256/1 NERC Understanding contemporary change in the West Antarctic ice sheet NE/E006108/1 NERC Not Set Not Set UK’s National Centre for Earth Observation cryosphere and climate themes - Keywords
- West Antarctic ice sheet; Pine Island Glacier; calibrated prediction; marine ice sheet instability; ice sheet modelling
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Copyright Holders
- © 2012 Elsevier
- Depositing User
- Tamsin Edwards