Past water flow beneath Pine Island and Thwaites glaciers, West Antarctica ...

• Main Authors: Kirkham, JD, Hogan, KA, Larter, RD, Arnold, NS, Nitsche, FO, Golledge, NR, Dowdeswell, JA
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus GmbH 2019
• Subjects: 37 Earth Sciences; 3709 Physical Geography and Environmental Geoscience; 3705 Geology; 13 Climate Action; Antarctic; Labyrinth; The Antarctic; West Antarctica; Antarc*; Antarctica; Ice Sheet; Pine Island
• Online Access: https://dx.doi.org/10.17863/cam.41963; https://www.repository.cam.ac.uk/handle/1810/294874

Abstract. Outburst floods from subglacial lakes beneath the Antarctic Ice Sheet modulate ice-flow velocities over periods of months to years. Although subglacial lake drainage events have been observed from satellite-altimetric data, little is known about their role in the long-term evolution of ice-sheet basal hydrology. Here, we systematically map and model past water flow through an extensive area containing over 1000 subglacial channels and 19 former lake basins exposed on over 19 000 km2 of seafloor by the retreat of Pine Island and Thwaites glaciers, West Antarctica. At 507 m wide and 43 m deep on average, the channels offshore of present-day Pine Island and Thwaites glaciers are approximately twice as deep, 3 times as wide, and cover an area over 400 times larger than the terrestrial meltwater channels comprising the Labyrinth in the Antarctic Dry Valleys. The channels incised into bedrock offshore of contemporary Pine Island and Thwaites glaciers would have been capable of accommodating discharges of ...