Ice stream motion facilitated by a shallow-deforming and accreting bed


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)
DOI: 10.1038/ncomms10723


7 Figures and Tables