Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b
With the rise of temperatures in the Arctic, Sentinel 1A and 1B data are used to examine the current state of Bylot Island's glaciers. This will provide valuable data for future sea-level and climate models to accurately predict the contribution the High Canadian Arctic has to sea-level rise. B...
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ftunicolboulder:oai:scholar.colorado.edu:geog_gradetds-1118 2023-05-15T13:11:14+02:00 Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b Bobeck, Jessica M. 2017-01-01T08:00:00Z application/pdf https://scholar.colorado.edu/geog_gradetds/117 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1118&context=geog_gradetds unknown CU Scholar https://scholar.colorado.edu/geog_gradetds/117 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1118&context=geog_gradetds Geography Graduate Theses & Dissertations climate change geophysics glacier velocity inSAR interferometry synthetic aperture radar Electrical and Computer Engineering Geophysics and Seismology Remote Sensing text 2017 ftunicolboulder 2018-10-07T09:07:39Z With the rise of temperatures in the Arctic, Sentinel 1A and 1B data are used to examine the current state of Bylot Island's glaciers. This will provide valuable data for future sea-level and climate models to accurately predict the contribution the High Canadian Arctic has to sea-level rise. Bylot Island is in a unique location in the High Canadian Arctic, as it sits on a transition zone between warming in the north and historical cooling to the south. By using Interferometric Synthetic Aperture Radar (InSAR), the three dimensional velocity vectors are calculated and used to produce horizontal velocity and melt loss maps for Bylot Island. Optical Feature Tracking is employed using Landsat 7 and Landsat 8 data to validate results and calculate Bylot Island's ice cap extent. Results show a decrease in overall glacier velocity, but increased glacier thinning from surface melt. Increased glacial thinning can be contributed to a Melt-Albedo positive feedback cycle. With melting beginning earlier each season, the overall extent of Bylot Island is rapidly decreasing and contributing more melt to sea-level than previously thought. Text albedo Arctic Bylot Island Climate change Ice cap University of Colorado, Boulder: CU Scholar Arctic Bylot Island |
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University of Colorado, Boulder: CU Scholar |
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ftunicolboulder |
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topic |
climate change geophysics glacier velocity inSAR interferometry synthetic aperture radar Electrical and Computer Engineering Geophysics and Seismology Remote Sensing |
spellingShingle |
climate change geophysics glacier velocity inSAR interferometry synthetic aperture radar Electrical and Computer Engineering Geophysics and Seismology Remote Sensing Bobeck, Jessica M. Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
topic_facet |
climate change geophysics glacier velocity inSAR interferometry synthetic aperture radar Electrical and Computer Engineering Geophysics and Seismology Remote Sensing |
description |
With the rise of temperatures in the Arctic, Sentinel 1A and 1B data are used to examine the current state of Bylot Island's glaciers. This will provide valuable data for future sea-level and climate models to accurately predict the contribution the High Canadian Arctic has to sea-level rise. Bylot Island is in a unique location in the High Canadian Arctic, as it sits on a transition zone between warming in the north and historical cooling to the south. By using Interferometric Synthetic Aperture Radar (InSAR), the three dimensional velocity vectors are calculated and used to produce horizontal velocity and melt loss maps for Bylot Island. Optical Feature Tracking is employed using Landsat 7 and Landsat 8 data to validate results and calculate Bylot Island's ice cap extent. Results show a decrease in overall glacier velocity, but increased glacier thinning from surface melt. Increased glacial thinning can be contributed to a Melt-Albedo positive feedback cycle. With melting beginning earlier each season, the overall extent of Bylot Island is rapidly decreasing and contributing more melt to sea-level than previously thought. |
format |
Text |
author |
Bobeck, Jessica M. |
author_facet |
Bobeck, Jessica M. |
author_sort |
Bobeck, Jessica M. |
title |
Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
title_short |
Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
title_full |
Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
title_fullStr |
Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
title_full_unstemmed |
Three Dimensional Glacier Flow of Bylot Island Derived Using Sentinel 1a and 1b |
title_sort |
three dimensional glacier flow of bylot island derived using sentinel 1a and 1b |
publisher |
CU Scholar |
publishDate |
2017 |
url |
https://scholar.colorado.edu/geog_gradetds/117 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1118&context=geog_gradetds |
geographic |
Arctic Bylot Island |
geographic_facet |
Arctic Bylot Island |
genre |
albedo Arctic Bylot Island Climate change Ice cap |
genre_facet |
albedo Arctic Bylot Island Climate change Ice cap |
op_source |
Geography Graduate Theses & Dissertations |
op_relation |
https://scholar.colorado.edu/geog_gradetds/117 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1118&context=geog_gradetds |
_version_ |
1766246469175607296 |