Characterization and interpretation of polythermal structure in two subarctic glaciers

I use ice-penetrating radar to probe the thermal structure in two small glaciers in the Saint Elias Range, southwestern Yukon. I develop processing workflows to separate bed and englacial reflections in radar and use these to build maps of both bed topography and englacial scattering. Comparison wit...

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Bibliographic Details
Main Author: Wilson, Nathaniel
Format: Thesis
Language:unknown
Published: 2012
Subjects:
Online Access:http://summit.sfu.ca/item/12553
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spelling ftsimonfu:oai:summit.sfu.ca:12553 2023-05-15T18:28:20+02:00 Characterization and interpretation of polythermal structure in two subarctic glaciers Wilson, Nathaniel 2012-11-29 http://summit.sfu.ca/item/12553 unknown etd7550 http://summit.sfu.ca/item/12553 Thesis 2012 ftsimonfu 2022-04-07T18:38:16Z I use ice-penetrating radar to probe the thermal structure in two small glaciers in the Saint Elias Range, southwestern Yukon. I develop processing workflows to separate bed and englacial reflections in radar and use these to build maps of both bed topography and englacial scattering. Comparison with borehole data shows that englacial scattering occurs in ice at the freezing point. The pattern in thermal structure suggests that the observed regime is dominated by accumulation zone processes. I develop a numerical model to simulate steady and time-dependent thermal regimes in glaciers. Diagnostic simulations support the hypothesis that meltwater entrapment is a critical control on the observed structure. Sensitivity tests suggest a climate sensitivity such that thinning and retreat of the near-surface aquifer may dramatically alter the thermal structure. Prognostic simulations illustrate scenarios in which these polythermal glaciers may cool as climate warms in the future. Thesis Subarctic Yukon Summit - SFU Research Repository (Simon Fraser University) Yukon
institution Open Polar
collection Summit - SFU Research Repository (Simon Fraser University)
op_collection_id ftsimonfu
language unknown
description I use ice-penetrating radar to probe the thermal structure in two small glaciers in the Saint Elias Range, southwestern Yukon. I develop processing workflows to separate bed and englacial reflections in radar and use these to build maps of both bed topography and englacial scattering. Comparison with borehole data shows that englacial scattering occurs in ice at the freezing point. The pattern in thermal structure suggests that the observed regime is dominated by accumulation zone processes. I develop a numerical model to simulate steady and time-dependent thermal regimes in glaciers. Diagnostic simulations support the hypothesis that meltwater entrapment is a critical control on the observed structure. Sensitivity tests suggest a climate sensitivity such that thinning and retreat of the near-surface aquifer may dramatically alter the thermal structure. Prognostic simulations illustrate scenarios in which these polythermal glaciers may cool as climate warms in the future.
format Thesis
author Wilson, Nathaniel
spellingShingle Wilson, Nathaniel
Characterization and interpretation of polythermal structure in two subarctic glaciers
author_facet Wilson, Nathaniel
author_sort Wilson, Nathaniel
title Characterization and interpretation of polythermal structure in two subarctic glaciers
title_short Characterization and interpretation of polythermal structure in two subarctic glaciers
title_full Characterization and interpretation of polythermal structure in two subarctic glaciers
title_fullStr Characterization and interpretation of polythermal structure in two subarctic glaciers
title_full_unstemmed Characterization and interpretation of polythermal structure in two subarctic glaciers
title_sort characterization and interpretation of polythermal structure in two subarctic glaciers
publishDate 2012
url http://summit.sfu.ca/item/12553
geographic Yukon
geographic_facet Yukon
genre Subarctic
Yukon
genre_facet Subarctic
Yukon
op_relation etd7550
http://summit.sfu.ca/item/12553
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