Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers
Surging and streaming of glaciers are modulated by meltwater availability and pressure which controls mechanical coupling at their beds. Using laboratory-scale experimental modelling and palaeoglaciological mapping, we explore how subglacial drainage landsystems control meltwater drainage efficiency...
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Cambridge University Press
2023
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Online Access: | https://doi.org/10.1017/jog.2022.107 https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65 |
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ftdoajarticles:oai:doaj.org/article:49b291ac6b6b4f6884e2bda11c064a65 2023-08-20T04:07:38+02:00 Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers Édouard Ravier Thomas Lelandais Jean Vérité Olivier Bourgeois 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.107 https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022001071/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.107 0022-1430 1727-5652 https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65 Journal of Glaciology, Vol 69, Pp 860-878 (2023) Drainage efficiency experimental modelling ice stream ice surge palaeoglaciology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.107 2023-07-30T00:36:44Z Surging and streaming of glaciers are modulated by meltwater availability and pressure which controls mechanical coupling at their beds. Using laboratory-scale experimental modelling and palaeoglaciological mapping, we explore how subglacial drainage landsystems control meltwater drainage efficiency and ice flow velocities for terrestrial-based ice lobes resting on flat horizontal and permeable beds. Two end-members regimes, surging and streaming, appear in our experiments. The surge regime is characterised by a rapid increase of drainage efficiency through development of tunnel valleys and their tributaries, thus reducing the duration of ice flow speed-up events by lowering water pressures and increasing ice-bed coupling. Tunnel valleys connected to ice lobe margins, submarginal thrust moraines, reduced ice lobe extensions and ephemeral shear margins are the most distinctive characteristics of this regime. The stream regime is characterised by disconnected channels of smaller dimensions unable to evacuate all the meltwater: this prolonged drainage inefficiency leads to sustained high ice flow velocity and steady shear margins. Small and rectilinear meltwater channels devoid of tributaries, often disconnected from ice lobe margins, and lineation swarms are diagnostic of this regime. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 19 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Drainage efficiency experimental modelling ice stream ice surge palaeoglaciology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Drainage efficiency experimental modelling ice stream ice surge palaeoglaciology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Édouard Ravier Thomas Lelandais Jean Vérité Olivier Bourgeois Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
topic_facet |
Drainage efficiency experimental modelling ice stream ice surge palaeoglaciology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Surging and streaming of glaciers are modulated by meltwater availability and pressure which controls mechanical coupling at their beds. Using laboratory-scale experimental modelling and palaeoglaciological mapping, we explore how subglacial drainage landsystems control meltwater drainage efficiency and ice flow velocities for terrestrial-based ice lobes resting on flat horizontal and permeable beds. Two end-members regimes, surging and streaming, appear in our experiments. The surge regime is characterised by a rapid increase of drainage efficiency through development of tunnel valleys and their tributaries, thus reducing the duration of ice flow speed-up events by lowering water pressures and increasing ice-bed coupling. Tunnel valleys connected to ice lobe margins, submarginal thrust moraines, reduced ice lobe extensions and ephemeral shear margins are the most distinctive characteristics of this regime. The stream regime is characterised by disconnected channels of smaller dimensions unable to evacuate all the meltwater: this prolonged drainage inefficiency leads to sustained high ice flow velocity and steady shear margins. Small and rectilinear meltwater channels devoid of tributaries, often disconnected from ice lobe margins, and lineation swarms are diagnostic of this regime. |
format |
Article in Journal/Newspaper |
author |
Édouard Ravier Thomas Lelandais Jean Vérité Olivier Bourgeois |
author_facet |
Édouard Ravier Thomas Lelandais Jean Vérité Olivier Bourgeois |
author_sort |
Édouard Ravier |
title |
Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
title_short |
Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
title_full |
Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
title_fullStr |
Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
title_full_unstemmed |
Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
title_sort |
variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers |
publisher |
Cambridge University Press |
publishDate |
2023 |
url |
https://doi.org/10.1017/jog.2022.107 https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 69, Pp 860-878 (2023) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143022001071/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.107 0022-1430 1727-5652 https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65 |
op_doi |
https://doi.org/10.1017/jog.2022.107 |
container_title |
Journal of Glaciology |
container_start_page |
1 |
op_container_end_page |
19 |
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1774719416858050560 |