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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Bibliographic Details
Main Author: Blade, Michelle
Other Authors: Moorman, Brian, Beauchamp, Benoit, Sjogren, Darren
Format: Master Thesis
Language:English
Published: Graduate Studies 2017
Subjects:
Physical Geography
icing
dam
lake
proglacial
spring
Arctic
emerging
polythermal
Bylot Island
Dam Lake
Dammed Lake
Online Access:http://hdl.handle.net/11023/4211
https://doi.org/10.11575/PRISM/25255

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