Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada

Abstract The variation in near‐surface ground‐ice content of the uppermost 1 m of permafrost was examined by drilling at 71 sites within the Kendall Island Bird Sanctuary of the outer Mackenzie Delta, Northwest Territories. Permafrost has aggraded in coastal low‐lying alluvial wetlands during the la...

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Published in:Permafrost and Periglacial Processes
Main Authors: Morse, P. D., Burn, C. R., Kokelj, S. V.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Ice
Online Access:http://dx.doi.org/10.1002/ppp.650
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.650
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spelling crwiley:10.1002/ppp.650 2024-09-15T18:11:22+00:00 Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada Morse, P. D. Burn, C. R. Kokelj, S. V. 2009 http://dx.doi.org/10.1002/ppp.650 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.650 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.650 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 2, page 155-171 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.650 2024-08-20T04:15:00Z Abstract The variation in near‐surface ground‐ice content of the uppermost 1 m of permafrost was examined by drilling at 71 sites within the Kendall Island Bird Sanctuary of the outer Mackenzie Delta, Northwest Territories. Permafrost has aggraded in coastal low‐lying alluvial wetlands during the last 1500 to 500 years, and high near‐surface ground‐ice contents have developed in this saturated environment. In contrast, the ground ice in upland terrain has accumulated since the early Holocene. Permafrost in these uplands has a mean excess‐ice content of 24%, lower than in the alluvial wetlands (34%), and ground‐ice distribution is inherently more variable in upland terrain than in lowlands. Gravimetric moisture content is statistically related to soil organic‐matter content, but the organic‐matter content confounds the relation between gravimetric moisture and excess‐ice content due to its low bulk density. Topographically controlled moisture availability and soil organic‐matter content are important to ground‐ice distribution in uplands, given the order of magnitude increase in gravimetric moisture contents downslope, and the occurrence of massive ice lenses over 50 cm thick at the base of slopes. The potential mean subsidence of alluvial wetlands due to thawing of the uppermost 1 m of permafrost is 34 cm. Such subsidence would substantially increase the frequency of flooding for portions of this area. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada. Article in Journal/Newspaper Ice Mackenzie Delta Northwest Territories permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 20 2 155 171
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The variation in near‐surface ground‐ice content of the uppermost 1 m of permafrost was examined by drilling at 71 sites within the Kendall Island Bird Sanctuary of the outer Mackenzie Delta, Northwest Territories. Permafrost has aggraded in coastal low‐lying alluvial wetlands during the last 1500 to 500 years, and high near‐surface ground‐ice contents have developed in this saturated environment. In contrast, the ground ice in upland terrain has accumulated since the early Holocene. Permafrost in these uplands has a mean excess‐ice content of 24%, lower than in the alluvial wetlands (34%), and ground‐ice distribution is inherently more variable in upland terrain than in lowlands. Gravimetric moisture content is statistically related to soil organic‐matter content, but the organic‐matter content confounds the relation between gravimetric moisture and excess‐ice content due to its low bulk density. Topographically controlled moisture availability and soil organic‐matter content are important to ground‐ice distribution in uplands, given the order of magnitude increase in gravimetric moisture contents downslope, and the occurrence of massive ice lenses over 50 cm thick at the base of slopes. The potential mean subsidence of alluvial wetlands due to thawing of the uppermost 1 m of permafrost is 34 cm. Such subsidence would substantially increase the frequency of flooding for portions of this area. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada.
format Article in Journal/Newspaper
author Morse, P. D.
Burn, C. R.
Kokelj, S. V.
spellingShingle Morse, P. D.
Burn, C. R.
Kokelj, S. V.
Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
author_facet Morse, P. D.
Burn, C. R.
Kokelj, S. V.
author_sort Morse, P. D.
title Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
title_short Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
title_full Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
title_fullStr Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
title_full_unstemmed Near‐surface ground‐ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada
title_sort near‐surface ground‐ice distribution, kendall island bird sanctuary, western arctic coast, canada
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/ppp.650
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.650
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.650
genre Ice
Mackenzie Delta
Northwest Territories
permafrost
Permafrost and Periglacial Processes
genre_facet Ice
Mackenzie Delta
Northwest Territories
permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 20, issue 2, page 155-171
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.650
container_title Permafrost and Periglacial Processes
container_volume 20
container_issue 2
container_start_page 155
op_container_end_page 171
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