Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...

Subglacial hydrologic systems regulate ice sheet flow, causing acceleration or deceleration, depending on hydraulic efficiency and the rate at which surface meltwater is delivered to the bed. Because these systems are rarely observed, ice sheet basal drainage represents a poorly integrated and uncer...

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Main Authors: Young, Tun, Christoffersen, Poul, Bougamont, Marion, Tulaczyk, Slawek M, Hubbard, Bryn, Mankoff, Kenneth D, Nicholls, Keith W, Stewart, Craig L
Format: Article in Journal/Newspaper
Language:English
Published: Proceedings of the National Academy of Sciences 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.78858
https://www.repository.cam.ac.uk/handle/1810/331405
id ftdatacite:10.17863/cam.78858
record_format openpolar
spelling ftdatacite:10.17863/cam.78858 2024-02-04T10:00:35+01:00 Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ... Young, Tun Christoffersen, Poul Bougamont, Marion Tulaczyk, Slawek M Hubbard, Bryn Mankoff, Kenneth D Nicholls, Keith W Stewart, Craig L 2022 https://dx.doi.org/10.17863/cam.78858 https://www.repository.cam.ac.uk/handle/1810/331405 en eng Proceedings of the National Academy of Sciences https://doi.org/10.17863/CAM.80852 open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Article ScholarlyArticle JournalArticle article-journal 2022 ftdatacite https://doi.org/10.17863/cam.78858 2024-01-05T10:03:29Z Subglacial hydrologic systems regulate ice sheet flow, causing acceleration or deceleration, depending on hydraulic efficiency and the rate at which surface meltwater is delivered to the bed. Because these systems are rarely observed, ice sheet basal drainage represents a poorly integrated and uncertain component of models used to predict sea level changes. Here, we report radar-derived basal melt rates and unexpectedly warm subglacial conditions beneath a large Greenlandic outlet glacier. The basal melt rates averaged 14 mm ⋅d-1 over 4 months, peaking at 57 mm ⋅d-1 when basal water temperature reached +0.88 ∘C in a nearby borehole. We attribute both observations to the conversion of potential energy of surface water to heat in the basal drainage system, which peaked during a period of rainfall and intense surface melting. Our findings reveal limitations in the theory of channel formation, and we show that viscous dissipation far surpasses other basal heat sources, even in a distributed, high-pressure system. ... Article in Journal/Newspaper glacier Greenland greenlandic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Subglacial hydrologic systems regulate ice sheet flow, causing acceleration or deceleration, depending on hydraulic efficiency and the rate at which surface meltwater is delivered to the bed. Because these systems are rarely observed, ice sheet basal drainage represents a poorly integrated and uncertain component of models used to predict sea level changes. Here, we report radar-derived basal melt rates and unexpectedly warm subglacial conditions beneath a large Greenlandic outlet glacier. The basal melt rates averaged 14 mm ⋅d-1 over 4 months, peaking at 57 mm ⋅d-1 when basal water temperature reached +0.88 ∘C in a nearby borehole. We attribute both observations to the conversion of potential energy of surface water to heat in the basal drainage system, which peaked during a period of rainfall and intense surface melting. Our findings reveal limitations in the theory of channel formation, and we show that viscous dissipation far surpasses other basal heat sources, even in a distributed, high-pressure system. ...
format Article in Journal/Newspaper
author Young, Tun
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek M
Hubbard, Bryn
Mankoff, Kenneth D
Nicholls, Keith W
Stewart, Craig L
spellingShingle Young, Tun
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek M
Hubbard, Bryn
Mankoff, Kenneth D
Nicholls, Keith W
Stewart, Craig L
Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
author_facet Young, Tun
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek M
Hubbard, Bryn
Mankoff, Kenneth D
Nicholls, Keith W
Stewart, Craig L
author_sort Young, Tun
title Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
title_short Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
title_full Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
title_fullStr Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
title_full_unstemmed Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage. ...
title_sort rapid basal melting of the greenland ice sheet from surface meltwater drainage. ...
publisher Proceedings of the National Academy of Sciences
publishDate 2022
url https://dx.doi.org/10.17863/cam.78858
https://www.repository.cam.ac.uk/handle/1810/331405
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
greenlandic
Ice Sheet
genre_facet glacier
Greenland
greenlandic
Ice Sheet
op_relation https://doi.org/10.17863/CAM.80852
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.78858
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