slumps on Herschel Island, Yukon Territory

Abstract. The western Canadian Arctic is identified as an area of potentially significant global warming. Thawing permafrost, sea level rise, changing sea ice conditions and increased wave activity will result in accelerated rates of coastal erosion and thermokarst activity in areas of ice-rich perm...

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Main Authors: H. Lantuit, W. H. Pollard
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.382.8502
http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.382.8502 2023-05-15T14:53:31+02:00 slumps on Herschel Island, Yukon Territory H. Lantuit W. H. Pollard The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.382.8502 http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.382.8502 http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf text ftciteseerx 2016-09-18T00:26:48Z Abstract. The western Canadian Arctic is identified as an area of potentially significant global warming. Thawing permafrost, sea level rise, changing sea ice conditions and increased wave activity will result in accelerated rates of coastal erosion and thermokarst activity in areas of ice-rich permafrost. The Yukon Coastal Plain is widely recognized as one of the most ice-rich and thaw-sensitive areas in the Canadian Arctic. In particular, Herschel Island displays extensive coastal thermokarst. Retrogressive thaw slumps are a common thermokarst landform along the Herschel Island coast that have been increasing in both frequency and extent have in recent years due to increased thawing of massive ground ice and coastal erosion. The volume of sediment and ground ice eroded by retrogressive slump activity and the potential release of climate change related materials like organic carbon, carbon dioxide and methane are largely unknown. The remote setting of Herschel Island, and the Arctic in general, make direct observation of this type of erosion and the analysis of potential climate feedbacks extremely problematic. Remote sensing provides possibly the best solution to this problem. This study looks at two retrogressive thaw slumps located on the western shore of Herschel Island and using stereophotogrammetric methods attempts to (1) develop the first three-dimensional geomorphic analysis of this type of landform, and (2) provide an estimation of the volume of sediment/ground ice eroded through back wasting thermokarst activity. Digital Elevation Models were extracted for the Text Arctic Climate change Global warming Herschel Herschel Island Ice permafrost Sea ice Thermokarst Yukon Unknown Arctic Herschel Island ENVELOPE(-139.089,-139.089,69.583,69.583) Yukon
institution Open Polar
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op_collection_id ftciteseerx
language English
description Abstract. The western Canadian Arctic is identified as an area of potentially significant global warming. Thawing permafrost, sea level rise, changing sea ice conditions and increased wave activity will result in accelerated rates of coastal erosion and thermokarst activity in areas of ice-rich permafrost. The Yukon Coastal Plain is widely recognized as one of the most ice-rich and thaw-sensitive areas in the Canadian Arctic. In particular, Herschel Island displays extensive coastal thermokarst. Retrogressive thaw slumps are a common thermokarst landform along the Herschel Island coast that have been increasing in both frequency and extent have in recent years due to increased thawing of massive ground ice and coastal erosion. The volume of sediment and ground ice eroded by retrogressive slump activity and the potential release of climate change related materials like organic carbon, carbon dioxide and methane are largely unknown. The remote setting of Herschel Island, and the Arctic in general, make direct observation of this type of erosion and the analysis of potential climate feedbacks extremely problematic. Remote sensing provides possibly the best solution to this problem. This study looks at two retrogressive thaw slumps located on the western shore of Herschel Island and using stereophotogrammetric methods attempts to (1) develop the first three-dimensional geomorphic analysis of this type of landform, and (2) provide an estimation of the volume of sediment/ground ice eroded through back wasting thermokarst activity. Digital Elevation Models were extracted for the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author H. Lantuit
W. H. Pollard
spellingShingle H. Lantuit
W. H. Pollard
slumps on Herschel Island, Yukon Territory
author_facet H. Lantuit
W. H. Pollard
author_sort H. Lantuit
title slumps on Herschel Island, Yukon Territory
title_short slumps on Herschel Island, Yukon Territory
title_full slumps on Herschel Island, Yukon Territory
title_fullStr slumps on Herschel Island, Yukon Territory
title_full_unstemmed slumps on Herschel Island, Yukon Territory
title_sort slumps on herschel island, yukon territory
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.382.8502
http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf
long_lat ENVELOPE(-139.089,-139.089,69.583,69.583)
geographic Arctic
Herschel Island
Yukon
geographic_facet Arctic
Herschel Island
Yukon
genre Arctic
Climate change
Global warming
Herschel
Herschel Island
Ice
permafrost
Sea ice
Thermokarst
Yukon
genre_facet Arctic
Climate change
Global warming
Herschel
Herschel Island
Ice
permafrost
Sea ice
Thermokarst
Yukon
op_source http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf
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http://hal.archives-ouvertes.fr/docs/00/29/91/96/PDF/nhess-5-413-2005.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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