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 uncertai...

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Main Authors: Young, Tun Jan, Christoffersen, Poul, Bougamont, Marion, Tulaczyk, Slawek, Mankoff, Kenneth, Nicholls, Keith, Stewart, Craig
Format: Article in Journal/Newspaper
Language:English
Published: National Academy of Sciences 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.82846
https://www.repository.cam.ac.uk/handle/1810/335417
id ftdatacite:10.17863/cam.82846
record_format openpolar
spelling ftdatacite:10.17863/cam.82846 2024-02-27T08:40:44+00:00 Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage ... Young, Tun Jan Christoffersen, Poul Bougamont, Marion Tulaczyk, Slawek Mankoff, Kenneth Nicholls, Keith Stewart, Craig 2022 https://dx.doi.org/10.17863/cam.82846 https://www.repository.cam.ac.uk/handle/1810/335417 en eng National Academy of Sciences open.access Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 Greenland climate change glaciology ice sheets radio echo sounding article-journal ScholarlyArticle JournalArticle Article 2022 ftdatacite https://doi.org/10.17863/cam.82846 2024-02-01T15:02:53Z 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 wa-ter temperature reached +0.88 C in a nearby borehole. We attribute both observations to the conversion of potential energy of surface water as 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
topic Greenland
climate change
glaciology
ice sheets
radio echo sounding
spellingShingle Greenland
climate change
glaciology
ice sheets
radio echo sounding
Young, Tun Jan
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek
Mankoff, Kenneth
Nicholls, Keith
Stewart, Craig
Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage ...
topic_facet Greenland
climate change
glaciology
ice sheets
radio echo sounding
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 wa-ter temperature reached +0.88 C in a nearby borehole. We attribute both observations to the conversion of potential energy of surface water as 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 Jan
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek
Mankoff, Kenneth
Nicholls, Keith
Stewart, Craig
author_facet Young, Tun Jan
Christoffersen, Poul
Bougamont, Marion
Tulaczyk, Slawek
Mankoff, Kenneth
Nicholls, Keith
Stewart, Craig
author_sort Young, Tun Jan
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 National Academy of Sciences
publishDate 2022
url https://dx.doi.org/10.17863/cam.82846
https://www.repository.cam.ac.uk/handle/1810/335417
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
greenlandic
Ice Sheet
genre_facet glacier
Greenland
greenlandic
Ice Sheet
op_rights open.access
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.82846
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