A multicomponent coupled model of glacier hydrology ...

Multiple lines of evidence suggest a causal link between subglacial hydrology and phenomena such as fast-flowing ice. This evidence includes a measured correlation between water under alpine glaciers and their motion, the presence of saturated sediment beneath Antarctic ice streams, and geologic sig...

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Main Author: Flowers, Gwenn Elizabeth
Format: Text
Language:English
Published: University of British Columbia 2009
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0053158
https://doi.library.ubc.ca/10.14288/1.0053158
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spelling ftdatacite:10.14288/1.0053158 2024-04-28T08:02:34+00:00 A multicomponent coupled model of glacier hydrology ... Flowers, Gwenn Elizabeth 2009 https://dx.doi.org/10.14288/1.0053158 https://doi.library.ubc.ca/10.14288/1.0053158 en eng University of British Columbia article-journal Text ScholarlyArticle 2009 ftdatacite https://doi.org/10.14288/1.0053158 2024-04-02T09:44:20Z Multiple lines of evidence suggest a causal link between subglacial hydrology and phenomena such as fast-flowing ice. This evidence includes a measured correlation between water under alpine glaciers and their motion, the presence of saturated sediment beneath Antarctic ice streams, and geologic signatures of enhanced paleo-ice flow over deformable substrates. The complexity of the glacier bed as a three-component mixture presents an obstacle to unraveling these conundra. Inadequate representations of hydrology, in part, prevent us from closing the gap between empirical descriptions and a comprehensive consistent framework for understanding the dynamics of glacierized systems. I have developed a distributed numerical model that solves equations governing glacier surface runoff, englacial water transport, subglacial drainage, and subsurface groundwater flow. Ablation and precipitation drive the surface model through a temperature-index parameterization. Water is permitted to flow over and off the glacier, or ... Text Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
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language English
description Multiple lines of evidence suggest a causal link between subglacial hydrology and phenomena such as fast-flowing ice. This evidence includes a measured correlation between water under alpine glaciers and their motion, the presence of saturated sediment beneath Antarctic ice streams, and geologic signatures of enhanced paleo-ice flow over deformable substrates. The complexity of the glacier bed as a three-component mixture presents an obstacle to unraveling these conundra. Inadequate representations of hydrology, in part, prevent us from closing the gap between empirical descriptions and a comprehensive consistent framework for understanding the dynamics of glacierized systems. I have developed a distributed numerical model that solves equations governing glacier surface runoff, englacial water transport, subglacial drainage, and subsurface groundwater flow. Ablation and precipitation drive the surface model through a temperature-index parameterization. Water is permitted to flow over and off the glacier, or ...
format Text
author Flowers, Gwenn Elizabeth
spellingShingle Flowers, Gwenn Elizabeth
A multicomponent coupled model of glacier hydrology ...
author_facet Flowers, Gwenn Elizabeth
author_sort Flowers, Gwenn Elizabeth
title A multicomponent coupled model of glacier hydrology ...
title_short A multicomponent coupled model of glacier hydrology ...
title_full A multicomponent coupled model of glacier hydrology ...
title_fullStr A multicomponent coupled model of glacier hydrology ...
title_full_unstemmed A multicomponent coupled model of glacier hydrology ...
title_sort multicomponent coupled model of glacier hydrology ...
publisher University of British Columbia
publishDate 2009
url https://dx.doi.org/10.14288/1.0053158
https://doi.library.ubc.ca/10.14288/1.0053158
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genre_facet Antarc*
Antarctic
op_doi https://doi.org/10.14288/1.0053158
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