K.A. Hogan
Subglacial Water Flow Over an Antarctic Palaeo‐Ice Stream Bed
Hogan, K.A.; Arnold, N.S.; Larter, R.D.; Kirkham, J.D.; Noormets, R.; Ó Cofaigh, C.; Golledge, N.R.; Dowdeswell, J.A.
Authors
N.S. Arnold
R.D. Larter
J.D. Kirkham
R. Noormets
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
N.R. Golledge
J.A. Dowdeswell
Abstract
The subglacial hydrological system exerts a critical control on the dynamic behavior of the overlying ice because its configuration affects the degree of basal lubrication between the ice and the bed. Yet, this component of the glaciological system is notoriously hard to access and observe, particularly over timescales longer than the satellite era. In Antarctica, abundant evidence for past subglacial water flow over former ice-sheet beds exists around the peripheries of the ice sheet including networks of huge channels carved into bedrock (now submarine) on the Pacific margin of West Antarctica. Here, we combine detailed bathymetric investigations of a channel system in Marguerite Trough, a major palaeo-ice stream bed, with numerical hydrological modeling to explore subglacial water accumulation, routing and potential for erosion over decadal-centennial timescales. Detailed channel morphologies from remotely operated vehicle surveys indicate multiple stages of localized incision, and the occurrence of potholes, some gigantic in scale, suggests incision by turbulent water carrying a significant bedload. Further, the modeling indicates that subglacial water is available during deglaciation and was likely released in episodic drainage events, from subglacial lakes, varying in magnitude over time. Our observations support previous assertions that these huge bedrock channel systems were incised over multiple glacial cycles through episodic subglacial lake drainage events; however, here we present a viable pattern for subglacial drainage at times when the ice sheet existed over the continental shelf and was capable of continuing to erode the bedrock substrate.
Citation
Hogan, K., Arnold, N., Larter, R., Kirkham, J., Noormets, R., Ó Cofaigh, C., Golledge, N., & Dowdeswell, J. (2022). Subglacial Water Flow Over an Antarctic Palaeo‐Ice Stream Bed. Journal of Geophysical Research: Earth Surface, 127(2), Article e2021JF006442. https://doi.org/10.1029/2021jf006442
Journal Article Type | Article |
---|---|
Acceptance Date | Jan 31, 2022 |
Online Publication Date | Feb 18, 2022 |
Publication Date | 2022-02 |
Deposit Date | Apr 13, 2022 |
Publicly Available Date | Apr 19, 2022 |
Journal | Journal of geophysical research. Earth surface. |
Print ISSN | 2169-9011 |
Electronic ISSN | 2169-9011 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 127 |
Issue | 2 |
Article Number | e2021JF006442 |
DOI | https://doi.org/10.1029/2021jf006442 |
Public URL | https://durham-repository.worktribe.com/output/1209811 |
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Copyright Statement
© 2022. The Authors.
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
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