Improved representation of laminar and turbulent sheet flow in subglacial drainage models

Abstract Subglacial hydrology models struggle to reproduce seasonal drainage patterns that are consistent with observed subglacial water pressures and surface velocities. We modify the standard sheet-flow parameterization within a coupled sheet–channel subglacial drainage model to smoothly transitio...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Hill, Tim, Flowers, Gwenn Elizabeth, Hoffman, Matthew James, Bingham, Derek, Werder, Mauro Angelo
Other Authors: Natural Sciences and Engineering Research Council of Canada
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2023.103
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300103X
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spelling crcambridgeupr:10.1017/jog.2023.103 2024-03-03T08:45:55+00:00 Improved representation of laminar and turbulent sheet flow in subglacial drainage models Hill, Tim Flowers, Gwenn Elizabeth Hoffman, Matthew James Bingham, Derek Werder, Mauro Angelo Natural Sciences and Engineering Research Council of Canada 2023 http://dx.doi.org/10.1017/jog.2023.103 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300103X en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by-nc-sa/4.0 Journal of Glaciology page 1-14 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2023.103 2024-02-08T08:32:27Z Abstract Subglacial hydrology models struggle to reproduce seasonal drainage patterns that are consistent with observed subglacial water pressures and surface velocities. We modify the standard sheet-flow parameterization within a coupled sheet–channel subglacial drainage model to smoothly transition between laminar and turbulent flow based on the locally computed Reynolds number in a physically consistent way (the ‘transition’ model). We compare the transition model to standard laminar and turbulent models to assess the role of the sheet-flow parameterization in reconciling observed and modelled water pressures under idealized and realistic forcing. Relative to the turbulent model, the laminar and transition models improve seasonal simulations by increasing winter water pressure and producing a more prominent late-summer water pressure minimum. In contrast to the laminar model, the transition model remains consistent with its own internal assumptions across all flow regimes. Based on the internal consistency of the transition model and its improved performance relative to the standard turbulent model, we recommend its use for transient simulations of subglacial drainage. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 14
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hill, Tim
Flowers, Gwenn Elizabeth
Hoffman, Matthew James
Bingham, Derek
Werder, Mauro Angelo
Improved representation of laminar and turbulent sheet flow in subglacial drainage models
topic_facet Earth-Surface Processes
description Abstract Subglacial hydrology models struggle to reproduce seasonal drainage patterns that are consistent with observed subglacial water pressures and surface velocities. We modify the standard sheet-flow parameterization within a coupled sheet–channel subglacial drainage model to smoothly transition between laminar and turbulent flow based on the locally computed Reynolds number in a physically consistent way (the ‘transition’ model). We compare the transition model to standard laminar and turbulent models to assess the role of the sheet-flow parameterization in reconciling observed and modelled water pressures under idealized and realistic forcing. Relative to the turbulent model, the laminar and transition models improve seasonal simulations by increasing winter water pressure and producing a more prominent late-summer water pressure minimum. In contrast to the laminar model, the transition model remains consistent with its own internal assumptions across all flow regimes. Based on the internal consistency of the transition model and its improved performance relative to the standard turbulent model, we recommend its use for transient simulations of subglacial drainage.
author2 Natural Sciences and Engineering Research Council of Canada
format Article in Journal/Newspaper
author Hill, Tim
Flowers, Gwenn Elizabeth
Hoffman, Matthew James
Bingham, Derek
Werder, Mauro Angelo
author_facet Hill, Tim
Flowers, Gwenn Elizabeth
Hoffman, Matthew James
Bingham, Derek
Werder, Mauro Angelo
author_sort Hill, Tim
title Improved representation of laminar and turbulent sheet flow in subglacial drainage models
title_short Improved representation of laminar and turbulent sheet flow in subglacial drainage models
title_full Improved representation of laminar and turbulent sheet flow in subglacial drainage models
title_fullStr Improved representation of laminar and turbulent sheet flow in subglacial drainage models
title_full_unstemmed Improved representation of laminar and turbulent sheet flow in subglacial drainage models
title_sort improved representation of laminar and turbulent sheet flow in subglacial drainage models
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2023.103
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300103X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
page 1-14
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by-nc-sa/4.0
op_doi https://doi.org/10.1017/jog.2023.103
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 14
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