Modelling channelized surface drainage of supraglacial lakes
Supraglacial lakes can drain to the bed of ice sheets, affecting ice dynamics, or over their surface, relocating surface water. Focusing on surface drainage, we first discuss observations of lake drainage. In particular, for the first time, lakes are observed to drain >70 km across the Nivlisen i...
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International Glaciological Society
2015
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Online Access: | https://eprints.whiterose.ac.uk/92054/ https://eprints.whiterose.ac.uk/92054/1/WRRO_92054.pdf https://doi.org/10.3189/2015JoG14J158 |
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ftleedsuniv:oai:eprints.whiterose.ac.uk:92054 2023-05-15T13:55:00+02:00 Modelling channelized surface drainage of supraglacial lakes Kingslake, J. Ng, F. Sole, A. 2015-02 text https://eprints.whiterose.ac.uk/92054/ https://eprints.whiterose.ac.uk/92054/1/WRRO_92054.pdf https://doi.org/10.3189/2015JoG14J158 en eng International Glaciological Society https://eprints.whiterose.ac.uk/92054/1/WRRO_92054.pdf Kingslake, J., Ng, F. and Sole, A. (2015) Modelling channelized surface drainage of supraglacial lakes. Journal of Glaciology, 61 (225). 185 - 199. ISSN 0022-1430 Article PeerReviewed 2015 ftleedsuniv https://doi.org/10.3189/2015JoG14J158 2023-01-30T21:36:52Z Supraglacial lakes can drain to the bed of ice sheets, affecting ice dynamics, or over their surface, relocating surface water. Focusing on surface drainage, we first discuss observations of lake drainage. In particular, for the first time, lakes are observed to drain >70 km across the Nivlisen ice shelf, East Antarctica. Inspired by these observations, we develop a model of lake drainage through a channel that incises into an ice-sheet surface by frictional heat dissipated in the flow. Modelled lake drainage can be stable or unstable. During stable drainage, the rate of lake-level drawdown exceeds the rate of channel incision, so discharge from the lake decreases with time; this can prevent the lake from emptying completely. During unstable drainage, discharge grows unstably with time and always empties the lake. Model lakes are more prone to drain unstably when the initial lake area, the lake input and the channel slope are larger. These parameters will vary during atmospheric-warming-induced ablation-area expansion, hence the mechanisms revealed by our analysis can influence the dynamic response of ice sheets to warming through their impact on surface-water routing and storage. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Journal of Glaciology White Rose Research Online (Universities of Leeds, Sheffield & York) East Antarctica Nivlisen ENVELOPE(11.000,11.000,-70.333,-70.333) Journal of Glaciology 61 225 185 199 |
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Open Polar |
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White Rose Research Online (Universities of Leeds, Sheffield & York) |
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ftleedsuniv |
language |
English |
description |
Supraglacial lakes can drain to the bed of ice sheets, affecting ice dynamics, or over their surface, relocating surface water. Focusing on surface drainage, we first discuss observations of lake drainage. In particular, for the first time, lakes are observed to drain >70 km across the Nivlisen ice shelf, East Antarctica. Inspired by these observations, we develop a model of lake drainage through a channel that incises into an ice-sheet surface by frictional heat dissipated in the flow. Modelled lake drainage can be stable or unstable. During stable drainage, the rate of lake-level drawdown exceeds the rate of channel incision, so discharge from the lake decreases with time; this can prevent the lake from emptying completely. During unstable drainage, discharge grows unstably with time and always empties the lake. Model lakes are more prone to drain unstably when the initial lake area, the lake input and the channel slope are larger. These parameters will vary during atmospheric-warming-induced ablation-area expansion, hence the mechanisms revealed by our analysis can influence the dynamic response of ice sheets to warming through their impact on surface-water routing and storage. |
format |
Article in Journal/Newspaper |
author |
Kingslake, J. Ng, F. Sole, A. |
spellingShingle |
Kingslake, J. Ng, F. Sole, A. Modelling channelized surface drainage of supraglacial lakes |
author_facet |
Kingslake, J. Ng, F. Sole, A. |
author_sort |
Kingslake, J. |
title |
Modelling channelized surface drainage of supraglacial lakes |
title_short |
Modelling channelized surface drainage of supraglacial lakes |
title_full |
Modelling channelized surface drainage of supraglacial lakes |
title_fullStr |
Modelling channelized surface drainage of supraglacial lakes |
title_full_unstemmed |
Modelling channelized surface drainage of supraglacial lakes |
title_sort |
modelling channelized surface drainage of supraglacial lakes |
publisher |
International Glaciological Society |
publishDate |
2015 |
url |
https://eprints.whiterose.ac.uk/92054/ https://eprints.whiterose.ac.uk/92054/1/WRRO_92054.pdf https://doi.org/10.3189/2015JoG14J158 |
long_lat |
ENVELOPE(11.000,11.000,-70.333,-70.333) |
geographic |
East Antarctica Nivlisen |
geographic_facet |
East Antarctica Nivlisen |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Journal of Glaciology |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Journal of Glaciology |
op_relation |
https://eprints.whiterose.ac.uk/92054/1/WRRO_92054.pdf Kingslake, J., Ng, F. and Sole, A. (2015) Modelling channelized surface drainage of supraglacial lakes. Journal of Glaciology, 61 (225). 185 - 199. ISSN 0022-1430 |
op_doi |
https://doi.org/10.3189/2015JoG14J158 |
container_title |
Journal of Glaciology |
container_volume |
61 |
container_issue |
225 |
container_start_page |
185 |
op_container_end_page |
199 |
_version_ |
1766261219852812288 |