Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory

This project presents regional velocity measurements for the eastern portion of the St. Elias Mountains, including the entire glaciated area of Kluane National Park, derived from speckle tracking of Radarsat-2 imagery acquired in winter 2011 and 2012. This technique uses a cross-correlation approach...

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Bibliographic Details
Main Author: Waechter, Alexandra
Format: Thesis
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/10393/30190
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record_format openpolar
spelling ftcanadathes:oai:collectionscanada.gc.ca:OOU.#10393/30190 2023-05-15T17:04:25+02:00 Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory Waechter, Alexandra 2013-11-21T21:46:53Z http://hdl.handle.net/10393/30190 en eng http://hdl.handle.net/10393/30190 Yukon Territory Kaskawulsh Glacier Hubbard Glacier St. Elias Icefield speckle tracking glacier velocity Radarsat-2 Thèse / Thesis 2013 ftcanadathes 2014-06-14T23:47:59Z This project presents regional velocity measurements for the eastern portion of the St. Elias Mountains, including the entire glaciated area of Kluane National Park, derived from speckle tracking of Radarsat-2 imagery acquired in winter 2011 and 2012. This technique uses a cross-correlation approach to determine the displacement of the ‘speckle’ pattern of radar phase returns between two repeat-pass images. Further reconstruction of past velocities is performed on a selection of key glaciers using feature tracking of Landsat-5 imagery, allowing for the investigation of variability in glacier motion on interannual and decadal time scales. The results of the analysis showed that there is a strong velocity gradient across the region reflecting high accumulation rates on the Pacific-facing slope of the mountain range. These glaciers may have velocities an order of magnitude greater than glaciers of a similar size on the landward slope. Interannual variability was high, both in relation to surge events, of which a number were identified, and variation of other unknown controls on glacier motion. A long-term trend of velocity decrease was observed on the Kaskawulsh Glacier when comparing the results of this analysis to work carried out in the 1960s, the pattern of which is broadly congruent to measurements of surface elevation change over a similar period. Thesis Kluane National Park Yukon Theses Canada/Thèses Canada (Library and Archives Canada) Hubbard Glacier ENVELOPE(-139.379,-139.379,60.344,60.344) Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Pacific Yukon
institution Open Polar
collection Theses Canada/Thèses Canada (Library and Archives Canada)
op_collection_id ftcanadathes
language English
topic Yukon Territory
Kaskawulsh Glacier
Hubbard Glacier
St. Elias Icefield
speckle tracking
glacier velocity
Radarsat-2
spellingShingle Yukon Territory
Kaskawulsh Glacier
Hubbard Glacier
St. Elias Icefield
speckle tracking
glacier velocity
Radarsat-2
Waechter, Alexandra
Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
topic_facet Yukon Territory
Kaskawulsh Glacier
Hubbard Glacier
St. Elias Icefield
speckle tracking
glacier velocity
Radarsat-2
description This project presents regional velocity measurements for the eastern portion of the St. Elias Mountains, including the entire glaciated area of Kluane National Park, derived from speckle tracking of Radarsat-2 imagery acquired in winter 2011 and 2012. This technique uses a cross-correlation approach to determine the displacement of the ‘speckle’ pattern of radar phase returns between two repeat-pass images. Further reconstruction of past velocities is performed on a selection of key glaciers using feature tracking of Landsat-5 imagery, allowing for the investigation of variability in glacier motion on interannual and decadal time scales. The results of the analysis showed that there is a strong velocity gradient across the region reflecting high accumulation rates on the Pacific-facing slope of the mountain range. These glaciers may have velocities an order of magnitude greater than glaciers of a similar size on the landward slope. Interannual variability was high, both in relation to surge events, of which a number were identified, and variation of other unknown controls on glacier motion. A long-term trend of velocity decrease was observed on the Kaskawulsh Glacier when comparing the results of this analysis to work carried out in the 1960s, the pattern of which is broadly congruent to measurements of surface elevation change over a similar period.
format Thesis
author Waechter, Alexandra
author_facet Waechter, Alexandra
author_sort Waechter, Alexandra
title Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
title_short Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
title_full Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
title_fullStr Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
title_full_unstemmed Regional Assessment of Glacier Motion in Kluane National Park, Yukon Territory
title_sort regional assessment of glacier motion in kluane national park, yukon territory
publishDate 2013
url http://hdl.handle.net/10393/30190
long_lat ENVELOPE(-139.379,-139.379,60.344,60.344)
ENVELOPE(-139.104,-139.104,60.749,60.749)
geographic Hubbard Glacier
Kaskawulsh Glacier
Pacific
Yukon
geographic_facet Hubbard Glacier
Kaskawulsh Glacier
Pacific
Yukon
genre Kluane National Park
Yukon
genre_facet Kluane National Park
Yukon
op_relation http://hdl.handle.net/10393/30190
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