Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...

Abstract. We investigate the subglacial hydrology of Store Glacier in West Greenland, using the open-source, full-Stokes model Elmer/Ice in a novel 3D application that includes a distributed water sheet, as well as discrete channelised drainage, and a 1D model to simulate submarine plumes at the cal...

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Main Authors: Cook, SJ, Christoffersen, P, Todd, J, Slater, D, Chauché, N
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2020
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.52516
https://www.repository.cam.ac.uk/handle/1810/305436
id ftdatacite:10.17863/cam.52516
record_format openpolar
spelling ftdatacite:10.17863/cam.52516 2024-06-09T07:46:09+00:00 Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ... Cook, SJ Christoffersen, P Todd, J Slater, D Chauché, N 2020 https://dx.doi.org/10.17863/cam.52516 https://www.repository.cam.ac.uk/handle/1810/305436 en eng Copernicus GmbH https://doi.org/10.17863/CAM.50345 https://doi.org/10.17863/CAM.50345 https://dx.doi.org/10.5194/tc-2019-104 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 3707 Hydrology 3709 Physical Geography and Environmental Geoscience 37 Earth Sciences 13 Climate Action JournalArticle ScholarlyArticle article-journal Article 2020 ftdatacite https://doi.org/10.17863/cam.5251610.5194/tc-2019-104 2024-05-13T13:52:34Z Abstract. We investigate the subglacial hydrology of Store Glacier in West Greenland, using the open-source, full-Stokes model Elmer/Ice in a novel 3D application that includes a distributed water sheet, as well as discrete channelised drainage, and a 1D model to simulate submarine plumes at the calving front. At first, we produce a baseline winter scenario with no surface meltwater. We then investigate the hydrological system during summer, focussing specifically on 2012 and 2017, which provide examples of high and low surface-meltwater inputs, respectively. We show that the common assumption of zero winter freshwater flux is invalid, and we find channels over 1 m2 in area occurring up to 5 km inland in winter. We also find that the production of water from friction and geothermal heat is sufficiently high to drive year-round plume activity, with ice-front melting averaging 0.15 m d−1. When the model is forced with seasonally averaged surface melt from summer, we show a hydrological system with significant ... Article in Journal/Newspaper glacier Greenland 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 3707 Hydrology
3709 Physical Geography and Environmental Geoscience
37 Earth Sciences
13 Climate Action
spellingShingle 3707 Hydrology
3709 Physical Geography and Environmental Geoscience
37 Earth Sciences
13 Climate Action
Cook, SJ
Christoffersen, P
Todd, J
Slater, D
Chauché, N
Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
topic_facet 3707 Hydrology
3709 Physical Geography and Environmental Geoscience
37 Earth Sciences
13 Climate Action
description Abstract. We investigate the subglacial hydrology of Store Glacier in West Greenland, using the open-source, full-Stokes model Elmer/Ice in a novel 3D application that includes a distributed water sheet, as well as discrete channelised drainage, and a 1D model to simulate submarine plumes at the calving front. At first, we produce a baseline winter scenario with no surface meltwater. We then investigate the hydrological system during summer, focussing specifically on 2012 and 2017, which provide examples of high and low surface-meltwater inputs, respectively. We show that the common assumption of zero winter freshwater flux is invalid, and we find channels over 1 m2 in area occurring up to 5 km inland in winter. We also find that the production of water from friction and geothermal heat is sufficiently high to drive year-round plume activity, with ice-front melting averaging 0.15 m d−1. When the model is forced with seasonally averaged surface melt from summer, we show a hydrological system with significant ...
format Article in Journal/Newspaper
author Cook, SJ
Christoffersen, P
Todd, J
Slater, D
Chauché, N
author_facet Cook, SJ
Christoffersen, P
Todd, J
Slater, D
Chauché, N
author_sort Cook, SJ
title Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
title_short Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
title_full Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
title_fullStr Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
title_full_unstemmed Coupled modelling of subglacial hydrology and calving-front melting at Store Glacier, West Greenland ...
title_sort coupled modelling of subglacial hydrology and calving-front melting at store glacier, west greenland ...
publisher Copernicus GmbH
publishDate 2020
url https://dx.doi.org/10.17863/cam.52516
https://www.repository.cam.ac.uk/handle/1810/305436
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
genre_facet glacier
Greenland
op_relation https://doi.org/10.17863/CAM.50345
https://doi.org/10.17863/CAM.50345
https://dx.doi.org/10.5194/tc-2019-104
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.5251610.5194/tc-2019-104
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