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...

Full description

Bibliographic Details
Main Author: Blade, Michelle
Format: Master Thesis
Language:English
Published: Graduate Studies 2017
Subjects:
dam
Online Access:https://dx.doi.org/10.11575/prism/25255
https://prism.ucalgary.ca/handle/11023/4211
id ftdatacite:10.11575/prism/25255
record_format openpolar
spelling 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
collection 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