Contrasting hydrological controls on bed properties during the acceleration of Pine Island Glacier, West Antarctica

In the Amundsen sector of West Antarctica, the flow of glaciers accelerates when intrusion of warm ocean water onto the continental shelf induces strong melting beneath ice shelves and thinning near the glacier’s grounding lines. Projecting the future of these glaciers is, however, hindered by a poo...

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Bibliographic Details
Main Authors: Bougamont, MH, Christoffersen, Poul, Nias, Isabel, Vaughan, DG, Smith, AM, Brisbourne, Alex
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2019
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/288564
https://doi.org/10.17863/CAM.35847