Incorporating modelled subglacial hydrology into inversions for basal drag
A key challenge in modelling coupled ice-flow–subglacial hydrology is initializing the state and parameters of the system. We address this problem by presenting a workflow for initializing these values at the start of a summer melt season. The workflow depends on running a subglacial hydrology model...
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Copernicus Publications
2017
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00007818 2023-05-15T18:32:32+02:00 Incorporating modelled subglacial hydrology into inversions for basal drag Koziol, Conrad P. Arnold, Neil 2017-12 electronic https://doi.org/10.5194/tc-11-2783-2017 https://noa.gwlb.de/receive/cop_mods_00007818 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007775/tc-11-2783-2017.pdf https://tc.copernicus.org/articles/11/2783/2017/tc-11-2783-2017.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-11-2783-2017 https://noa.gwlb.de/receive/cop_mods_00007818 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007775/tc-11-2783-2017.pdf https://tc.copernicus.org/articles/11/2783/2017/tc-11-2783-2017.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2017 ftnonlinearchiv https://doi.org/10.5194/tc-11-2783-2017 2022-02-08T22:58:19Z A key challenge in modelling coupled ice-flow–subglacial hydrology is initializing the state and parameters of the system. We address this problem by presenting a workflow for initializing these values at the start of a summer melt season. The workflow depends on running a subglacial hydrology model for the winter season, when the system is not forced by meltwater inputs, and ice velocities can be assumed constant. Key parameters of the winter run of the subglacial hydrology model are determined from an initial inversion for basal drag using a linear sliding law. The state of the subglacial hydrology model at the end of winter is incorporated into an inversion of basal drag using a non-linear sliding law which is a function of water pressure. We demonstrate this procedure in the Russell Glacier area and compare the output of the linear sliding law with two non-linear sliding laws. Additionally, we compare the modelled winter hydrological state to radar observations and find that it is in line with summer rather than winter observations. Article in Journal/Newspaper The Cryosphere Niedersächsisches Online-Archiv NOA The Cryosphere 11 6 2783 2797 |
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article Verlagsveröffentlichung Koziol, Conrad P. Arnold, Neil Incorporating modelled subglacial hydrology into inversions for basal drag |
topic_facet |
article Verlagsveröffentlichung |
description |
A key challenge in modelling coupled ice-flow–subglacial hydrology is initializing the state and parameters of the system. We address this problem by presenting a workflow for initializing these values at the start of a summer melt season. The workflow depends on running a subglacial hydrology model for the winter season, when the system is not forced by meltwater inputs, and ice velocities can be assumed constant. Key parameters of the winter run of the subglacial hydrology model are determined from an initial inversion for basal drag using a linear sliding law. The state of the subglacial hydrology model at the end of winter is incorporated into an inversion of basal drag using a non-linear sliding law which is a function of water pressure. We demonstrate this procedure in the Russell Glacier area and compare the output of the linear sliding law with two non-linear sliding laws. Additionally, we compare the modelled winter hydrological state to radar observations and find that it is in line with summer rather than winter observations. |
format |
Article in Journal/Newspaper |
author |
Koziol, Conrad P. Arnold, Neil |
author_facet |
Koziol, Conrad P. Arnold, Neil |
author_sort |
Koziol, Conrad P. |
title |
Incorporating modelled subglacial hydrology into inversions for basal drag |
title_short |
Incorporating modelled subglacial hydrology into inversions for basal drag |
title_full |
Incorporating modelled subglacial hydrology into inversions for basal drag |
title_fullStr |
Incorporating modelled subglacial hydrology into inversions for basal drag |
title_full_unstemmed |
Incorporating modelled subglacial hydrology into inversions for basal drag |
title_sort |
incorporating modelled subglacial hydrology into inversions for basal drag |
publisher |
Copernicus Publications |
publishDate |
2017 |
url |
https://doi.org/10.5194/tc-11-2783-2017 https://noa.gwlb.de/receive/cop_mods_00007818 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007775/tc-11-2783-2017.pdf https://tc.copernicus.org/articles/11/2783/2017/tc-11-2783-2017.pdf |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_relation |
The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-11-2783-2017 https://noa.gwlb.de/receive/cop_mods_00007818 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007775/tc-11-2783-2017.pdf https://tc.copernicus.org/articles/11/2783/2017/tc-11-2783-2017.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/tc-11-2783-2017 |
container_title |
The Cryosphere |
container_volume |
11 |
container_issue |
6 |
container_start_page |
2783 |
op_container_end_page |
2797 |
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