Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...

AbstractThe 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,...

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Main Authors: Hogan, KA, Arnold, NS, Larter, RD, Kirkham, JD, Noormets, R, Ó Cofaigh, C, Golledge, NR, Dowdeswell, JA
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.81607
https://www.repository.cam.ac.uk/handle/1810/334195
id ftdatacite:10.17863/cam.81607
record_format openpolar
spelling ftdatacite:10.17863/cam.81607 2024-02-27T08:35:06+00:00 Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ... Hogan, KA Arnold, NS Larter, RD Kirkham, JD Noormets, R Ó Cofaigh, C Golledge, NR Dowdeswell, JA 2022 https://dx.doi.org/10.17863/cam.81607 https://www.repository.cam.ac.uk/handle/1810/334195 en eng American Geophysical Union (AGU) palaeo-ice stream subglacial hydrology bedrock channels Antarctica subglacial lakes marine geophysics article-journal ScholarlyArticle JournalArticle Article 2022 ftdatacite https://doi.org/10.17863/cam.81607 2024-02-01T15:02:50Z AbstractThe 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 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Pacific West Antarctica
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic palaeo-ice stream
subglacial hydrology
bedrock channels
Antarctica
subglacial lakes
marine geophysics
spellingShingle palaeo-ice stream
subglacial hydrology
bedrock channels
Antarctica
subglacial lakes
marine geophysics
Hogan, KA
Arnold, NS
Larter, RD
Kirkham, JD
Noormets, R
Ó Cofaigh, C
Golledge, NR
Dowdeswell, JA
Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
topic_facet palaeo-ice stream
subglacial hydrology
bedrock channels
Antarctica
subglacial lakes
marine geophysics
description AbstractThe 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 ...
format Article in Journal/Newspaper
author Hogan, KA
Arnold, NS
Larter, RD
Kirkham, JD
Noormets, R
Ó Cofaigh, C
Golledge, NR
Dowdeswell, JA
author_facet Hogan, KA
Arnold, NS
Larter, RD
Kirkham, JD
Noormets, R
Ó Cofaigh, C
Golledge, NR
Dowdeswell, JA
author_sort Hogan, KA
title Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
title_short Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
title_full Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
title_fullStr Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
title_full_unstemmed Subglacial Water Flow Over an Antarctic Palaeo-Ice Stream Bed ...
title_sort subglacial water flow over an antarctic palaeo-ice stream bed ...
publisher American Geophysical Union (AGU)
publishDate 2022
url https://dx.doi.org/10.17863/cam.81607
https://www.repository.cam.ac.uk/handle/1810/334195
long_lat ENVELOPE(141.378,141.378,-66.787,-66.787)
geographic Antarctic
Marguerite
Pacific
West Antarctica
geographic_facet Antarctic
Marguerite
Pacific
West Antarctica
genre Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
op_doi https://doi.org/10.17863/cam.81607
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