Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting
Computer models are necessary for understanding and predicting marine ice sheet behaviour. However, there is uncertainty over implementation of physical processes at the ice base, both for grounded and floating glacial ice. Here we implement several sliding relations in a marine ice sheet flow-line...
Published in: | The Cryosphere |
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Language: | English |
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Online Access: | https://doi.org/10.5194/tc-11-319-2017 https://tc.copernicus.org/articles/11/319/2017/ |
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ftcopernicus:oai:publications.copernicus.org:tc52435 2023-05-15T16:40:19+02:00 Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting Gladstone, Rupert Michael Warner, Roland Charles Galton-Fenzi, Benjamin Keith Gagliardini, Olivier Zwinger, Thomas Greve, Ralf 2018-09-27 info:eu-repo/semantics/application/pdf https://doi.org/10.5194/tc-11-319-2017 https://tc.copernicus.org/articles/11/319/2017/ eng eng info:eu-repo/grantAgreement/EC/FP7/299035 doi:10.5194/tc-11-319-2017 https://tc.copernicus.org/articles/11/319/2017/ info:eu-repo/semantics/openAccess eISSN: 1994-0424 info:eu-repo/semantics/Text 2018 ftcopernicus https://doi.org/10.5194/tc-11-319-2017 2020-07-20T16:23:51Z Computer models are necessary for understanding and predicting marine ice sheet behaviour. However, there is uncertainty over implementation of physical processes at the ice base, both for grounded and floating glacial ice. Here we implement several sliding relations in a marine ice sheet flow-line model accounting for all stress components and demonstrate that model resolution requirements are strongly dependent on both the choice of basal sliding relation and the spatial distribution of ice shelf basal melting. Sliding relations that reduce the magnitude of the step change in basal drag from grounded ice to floating ice (where basal drag is set to zero) show reduced dependence on resolution compared to a commonly used relation, in which basal drag is purely a power law function of basal ice velocity. Sliding relations in which basal drag goes smoothly to zero as the grounding line is approached from inland (due to a physically motivated incorporation of effective pressure at the bed) provide further reduction in resolution dependence. A similar issue is found with the imposition of basal melt under the floating part of the ice shelf: melt parameterisations that reduce the abruptness of change in basal melting from grounded ice (where basal melt is set to zero) to floating ice provide improved convergence with resolution compared to parameterisations in which high melt occurs adjacent to the grounding line. Thus physical processes, such as sub-glacial outflow (which could cause high melt near the grounding line), impact on capability to simulate marine ice sheets. If there exists an abrupt change across the grounding line in either basal drag or basal melting, then high resolution will be required to solve the problem. However, the plausible combination of a physical dependency of basal drag on effective pressure, and the possibility of low ice shelf basal melt rates next to the grounding line, may mean that some marine ice sheet systems can be reliably simulated at a coarser resolution than currently thought necessary. Other/Unknown Material Ice Sheet Ice Shelf Copernicus Publications: E-Journals The Cryosphere 11 1 319 329 |
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Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
Computer models are necessary for understanding and predicting marine ice sheet behaviour. However, there is uncertainty over implementation of physical processes at the ice base, both for grounded and floating glacial ice. Here we implement several sliding relations in a marine ice sheet flow-line model accounting for all stress components and demonstrate that model resolution requirements are strongly dependent on both the choice of basal sliding relation and the spatial distribution of ice shelf basal melting. Sliding relations that reduce the magnitude of the step change in basal drag from grounded ice to floating ice (where basal drag is set to zero) show reduced dependence on resolution compared to a commonly used relation, in which basal drag is purely a power law function of basal ice velocity. Sliding relations in which basal drag goes smoothly to zero as the grounding line is approached from inland (due to a physically motivated incorporation of effective pressure at the bed) provide further reduction in resolution dependence. A similar issue is found with the imposition of basal melt under the floating part of the ice shelf: melt parameterisations that reduce the abruptness of change in basal melting from grounded ice (where basal melt is set to zero) to floating ice provide improved convergence with resolution compared to parameterisations in which high melt occurs adjacent to the grounding line. Thus physical processes, such as sub-glacial outflow (which could cause high melt near the grounding line), impact on capability to simulate marine ice sheets. If there exists an abrupt change across the grounding line in either basal drag or basal melting, then high resolution will be required to solve the problem. However, the plausible combination of a physical dependency of basal drag on effective pressure, and the possibility of low ice shelf basal melt rates next to the grounding line, may mean that some marine ice sheet systems can be reliably simulated at a coarser resolution than currently thought necessary. |
format |
Other/Unknown Material |
author |
Gladstone, Rupert Michael Warner, Roland Charles Galton-Fenzi, Benjamin Keith Gagliardini, Olivier Zwinger, Thomas Greve, Ralf |
spellingShingle |
Gladstone, Rupert Michael Warner, Roland Charles Galton-Fenzi, Benjamin Keith Gagliardini, Olivier Zwinger, Thomas Greve, Ralf Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
author_facet |
Gladstone, Rupert Michael Warner, Roland Charles Galton-Fenzi, Benjamin Keith Gagliardini, Olivier Zwinger, Thomas Greve, Ralf |
author_sort |
Gladstone, Rupert Michael |
title |
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
title_short |
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
title_full |
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
title_fullStr |
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
title_full_unstemmed |
Marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
title_sort |
marine ice sheet model performance depends on basal sliding physics and sub-shelf melting |
publishDate |
2018 |
url |
https://doi.org/10.5194/tc-11-319-2017 https://tc.copernicus.org/articles/11/319/2017/ |
genre |
Ice Sheet Ice Shelf |
genre_facet |
Ice Sheet Ice Shelf |
op_source |
eISSN: 1994-0424 |
op_relation |
info:eu-repo/grantAgreement/EC/FP7/299035 doi:10.5194/tc-11-319-2017 https://tc.copernicus.org/articles/11/319/2017/ |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-11-319-2017 |
container_title |
The Cryosphere |
container_volume |
11 |
container_issue |
1 |
container_start_page |
319 |
op_container_end_page |
329 |
_version_ |
1766030705125490688 |