Jeremy C. Ely

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Ice streams drain large portions of ice sheets and play a fundamental role in governing their response to atmospheric and oceanic forcing, with implications for sea-level change. The mechanisms that generate ice stream flow remain elusive. Basal sliding and/or bed deformation have been hypothesized, but ice stream beds are largely inaccessible. Here we(More)
a Department of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK b Department of Geography, University of Sheffield, Sheffield S10 2TN, UK c School of Environmental Sciences, University of Liverpool, Liverpool L69 3GP, UK d Department of Geography and Earth Sciences, Aberystwyth University, Ceredigion SY23 3DB, UK e Scottish(More)
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