Temporal stereophotogrammetric analysis of retrogressive thaw slumps on Herschel Island, Yukon Territory

International audience 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...

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Bibliographic Details
Main Authors: Lantuit, H., Pollard, W. H.
Other Authors: Department of Geography Montréal, McGill University = Université McGill Montréal, Canada
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2005
Subjects:
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Arctic
Yukon
Herschel Island
Climate change
Global warming
Herschel
Ice
permafrost
Sea ice
Thermokarst
Online Access:https://hal.science/hal-00299196
https://hal.science/hal-00299196/document
https://hal.science/hal-00299196/file/nhess-5-413-2005.pdf

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