journal article Mar 07, 2017

East Antarctic ice sheet most vulnerable to Weddell Sea warming

View at Publisher Save 10.1002/2016gl072422
Abstract
AbstractModels predict considerable spatial variability in the magnitude of future climate change around Antarctica, suggesting that some sectors of the continent may be more affected by these changes than others. Furthermore, the geometry of the bedrock topography underlying the East and West Antarctic ice sheets, together with regional differences in ice thickness, mean that certain ice drainage basins may respond more or less sensitively to environmental forcings. Here we use an ensemble of idealized climates to drive ice‐sheet simulations that explore regional and continental‐scale thresholds, allowing us to identify a hierarchy of catchment vulnerabilities based on differences in long‐term catchment‐averaged ice loss. Considering this hierarchy in the context of recent observations and climate scenarios forecast for 2100 CE, we conclude that the majority of future ice loss from East Antarctica, both this century and over subsequent millennia, will likely come from the Recovery subglacial basin in the eastern Weddell Sea.
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Cited By
78
The hysteresis of the Antarctic Ice Sheet

Julius Garbe, Torsten Albrecht · 2020

Nature
Nature Climate Change
Metrics
78
Citations
37
References
Details
Published
Mar 07, 2017
Vol/Issue
44(5)
Pages
2343-2351
License
View
Funding
National Aeronautics and Space Administration Award: NNX13AM16G
Royal Society of New Zealand Award: RDF-VUW1501
Georgian National Science Foundation
Cite This Article
N. R. Golledge, R. H. Levy, R. M. McKay, et al. (2017). East Antarctic ice sheet most vulnerable to Weddell Sea warming. Geophysical Research Letters, 44(5), 2343-2351. https://doi.org/10.1002/2016gl072422
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