Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream

Basal hydrological systems play an important role in controlling the dynamic behaviour of ice streams. Data showing their morphology and relationship to geological substrates beneath modern ice streams are, however, sparse and difficult to collect. We present new multibeam bathymetry data that make...

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Main Authors: Larter, RD, Hogan, KA, Hillenbrand, CD, Smith, JA, Batchelor, CL, Cartigny, M, Tate, AJ, Kirkham, JD, Roseby, ZA, Kuhn, G, Graham, AGC, Dowdeswell, JA
Format: Article in Journal/Newspaper
Language:English
Published: EGU 2019
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/294282
https://doi.org/10.17863/CAM.41381
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spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/294282 2024-01-14T10:01:33+01:00 Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream Larter, RD Hogan, KA Hillenbrand, CD Smith, JA Batchelor, CL Cartigny, M Tate, AJ Kirkham, JD Roseby, ZA Kuhn, G Graham, AGC Dowdeswell, JA 2019-06-05 application/pdf https://www.repository.cam.ac.uk/handle/1810/294282 https://doi.org/10.17863/CAM.41381 eng eng EGU https://www.the-cryosphere.net/13/1583/2019/#section7 Cryosphere https://www.repository.cam.ac.uk/handle/1810/294282 doi:10.17863/CAM.41381 Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3702 Climate Change Science 3705 Geology Article 2019 ftunivcam https://doi.org/10.17863/CAM.41381 2023-12-21T23:20:17Z Basal hydrological systems play an important role in controlling the dynamic behaviour of ice streams. Data showing their morphology and relationship to geological substrates beneath modern ice streams are, however, sparse and difficult to collect. We present new multibeam bathymetry data that make the Anvers-Hugo Trough west of the Antarctic Peninsula the most completely surveyed palaeo-ice stream pathway in Antarctica. The data reveal a diverse range of landforms, including streamlined features where there was fast flow in the palaeo-ice stream, channels eroded by flow of subglacial water, and compelling evidence of palaeo-ice stream shear margin locations. We interpret landforms as indicating that subglacial water availability played an important role in facilitating ice stream flow and controlling shear margin positions. Water was likely supplied to the ice stream bed episodically as a result of outbursts from a subglacial lake located in the Palmer Deep basin on the inner continental shelf. These interpretations have implications for controls on the onset of fast ice flow, the dynamic behaviour of palaeo-ice streams on the Antarctic continental shelf, and potentially also for behaviour of modern ice streams. This research has been supported by the British Antarctic Survey, Natural Environment Research Council, Polar Science for Planet Earth programme. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica British Antarctic Survey Apollo - University of Cambridge Repository Antarctic Antarctic Peninsula Anvers ENVELOPE(-63.500,-63.500,-64.600,-64.600) Palmer Deep ENVELOPE(-64.400,-64.400,-64.950,-64.950) The Antarctic
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language English
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3702 Climate Change Science
3705 Geology
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3702 Climate Change Science
3705 Geology
Larter, RD
Hogan, KA
Hillenbrand, CD
Smith, JA
Batchelor, CL
Cartigny, M
Tate, AJ
Kirkham, JD
Roseby, ZA
Kuhn, G
Graham, AGC
Dowdeswell, JA
Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3702 Climate Change Science
3705 Geology
description Basal hydrological systems play an important role in controlling the dynamic behaviour of ice streams. Data showing their morphology and relationship to geological substrates beneath modern ice streams are, however, sparse and difficult to collect. We present new multibeam bathymetry data that make the Anvers-Hugo Trough west of the Antarctic Peninsula the most completely surveyed palaeo-ice stream pathway in Antarctica. The data reveal a diverse range of landforms, including streamlined features where there was fast flow in the palaeo-ice stream, channels eroded by flow of subglacial water, and compelling evidence of palaeo-ice stream shear margin locations. We interpret landforms as indicating that subglacial water availability played an important role in facilitating ice stream flow and controlling shear margin positions. Water was likely supplied to the ice stream bed episodically as a result of outbursts from a subglacial lake located in the Palmer Deep basin on the inner continental shelf. These interpretations have implications for controls on the onset of fast ice flow, the dynamic behaviour of palaeo-ice streams on the Antarctic continental shelf, and potentially also for behaviour of modern ice streams. This research has been supported by the British Antarctic Survey, Natural Environment Research Council, Polar Science for Planet Earth programme.
format Article in Journal/Newspaper
author Larter, RD
Hogan, KA
Hillenbrand, CD
Smith, JA
Batchelor, CL
Cartigny, M
Tate, AJ
Kirkham, JD
Roseby, ZA
Kuhn, G
Graham, AGC
Dowdeswell, JA
author_facet Larter, RD
Hogan, KA
Hillenbrand, CD
Smith, JA
Batchelor, CL
Cartigny, M
Tate, AJ
Kirkham, JD
Roseby, ZA
Kuhn, G
Graham, AGC
Dowdeswell, JA
author_sort Larter, RD
title Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
title_short Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
title_full Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
title_fullStr Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
title_full_unstemmed Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream
title_sort subglacial hydrological control on flow of an antarctic peninsula palaeo-ice stream
publisher EGU
publishDate 2019
url https://www.repository.cam.ac.uk/handle/1810/294282
https://doi.org/10.17863/CAM.41381
long_lat ENVELOPE(-63.500,-63.500,-64.600,-64.600)
ENVELOPE(-64.400,-64.400,-64.950,-64.950)
geographic Antarctic
Antarctic Peninsula
Anvers
Palmer Deep
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Anvers
Palmer Deep
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
British Antarctic Survey
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
British Antarctic Survey
op_relation https://www.repository.cam.ac.uk/handle/1810/294282
doi:10.17863/CAM.41381
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.17863/CAM.41381
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