Characteristics of an Icing-Dammed Proglacial Lake ...
Icing-dammed proglacial lakes form as a result of water-flow pathway restrictions caused by freezing of winter baseflow. With the majority of glaciers in the eastern Canadian High Arctic that previously terminated at sea level now terminating on land (Vaughan et al., 2013), emerging proglacial envir...
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2017
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Online Access: | https://dx.doi.org/10.11575/prism/25255 https://prism.ucalgary.ca/handle/11023/4211 |
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ftdatacite:10.11575/prism/25255 2023-11-05T03:38:50+01:00 Characteristics of an Icing-Dammed Proglacial Lake ... Blade, Michelle 2017 https://dx.doi.org/10.11575/prism/25255 https://prism.ucalgary.ca/handle/11023/4211 en eng Graduate Studies University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Physical Geography icing dam lake proglacial spring Arctic emerging polythermal article master thesis CreativeWork Other 2017 ftdatacite https://doi.org/10.11575/prism/25255 2023-10-09T10:52:29Z Icing-dammed proglacial lakes form as a result of water-flow pathway restrictions caused by freezing of winter baseflow. With the majority of glaciers in the eastern Canadian High Arctic that previously terminated at sea level now terminating on land (Vaughan et al., 2013), emerging proglacial environments are becoming more common - resulting in the occurrence of novel terrestrial proglacial water flow regimes. This research addressed the knowledge gap of how a glacier, proglacial environment, and hydrological cycle contribute to delayed water-flow, in the form of a proglacial icing-dammed lake, in the terrestrial proglacial environment. The research was conducted at a unique location on Bylot Island, NU, in the eastern Canadian High Arctic, where icing-dammed proglacial lakes have been observed to form multiple years prior. In the proglacial environment, icing development has been studied as proxies to infer winter baseflow from upvalley glacial hydrological networks (Hodgkins et al., 2004; Wainstein, ... Master Thesis Arctic Bylot Island DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Physical Geography icing dam lake proglacial spring Arctic emerging polythermal |
spellingShingle |
Physical Geography icing dam lake proglacial spring Arctic emerging polythermal Blade, Michelle Characteristics of an Icing-Dammed Proglacial Lake ... |
topic_facet |
Physical Geography icing dam lake proglacial spring Arctic emerging polythermal |
description |
Icing-dammed proglacial lakes form as a result of water-flow pathway restrictions caused by freezing of winter baseflow. With the majority of glaciers in the eastern Canadian High Arctic that previously terminated at sea level now terminating on land (Vaughan et al., 2013), emerging proglacial environments are becoming more common - resulting in the occurrence of novel terrestrial proglacial water flow regimes. This research addressed the knowledge gap of how a glacier, proglacial environment, and hydrological cycle contribute to delayed water-flow, in the form of a proglacial icing-dammed lake, in the terrestrial proglacial environment. The research was conducted at a unique location on Bylot Island, NU, in the eastern Canadian High Arctic, where icing-dammed proglacial lakes have been observed to form multiple years prior. In the proglacial environment, icing development has been studied as proxies to infer winter baseflow from upvalley glacial hydrological networks (Hodgkins et al., 2004; Wainstein, ... |
format |
Master Thesis |
author |
Blade, Michelle |
author_facet |
Blade, Michelle |
author_sort |
Blade, Michelle |
title |
Characteristics of an Icing-Dammed Proglacial Lake ... |
title_short |
Characteristics of an Icing-Dammed Proglacial Lake ... |
title_full |
Characteristics of an Icing-Dammed Proglacial Lake ... |
title_fullStr |
Characteristics of an Icing-Dammed Proglacial Lake ... |
title_full_unstemmed |
Characteristics of an Icing-Dammed Proglacial Lake ... |
title_sort |
characteristics of an icing-dammed proglacial lake ... |
publisher |
Graduate Studies |
publishDate |
2017 |
url |
https://dx.doi.org/10.11575/prism/25255 https://prism.ucalgary.ca/handle/11023/4211 |
genre |
Arctic Bylot Island |
genre_facet |
Arctic Bylot Island |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/prism/25255 |
_version_ |
1781694593487601664 |