Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories

Abstract Surface conditions and ground temperatures from 50‐cm to 20‐m depth were measured at 26 forested sites in the Mackenzie Delta, to determine if differences in forest structure and organic cover between four common white spruce forest community types were associated with variations in ground...

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Published in:Permafrost and Periglacial Processes
Main Authors: Kanigan, J. C. N., Burn, C. R., Kokelj, S. V.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.643
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spelling crwiley:10.1002/ppp.643 2024-06-02T08:05:39+00:00 Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories Kanigan, J. C. N. Burn, C. R. Kokelj, S. V. 2009 http://dx.doi.org/10.1002/ppp.643 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.643 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.643 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 2, page 127-139 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.643 2024-05-03T11:40:35Z Abstract Surface conditions and ground temperatures from 50‐cm to 20‐m depth were measured at 26 forested sites in the Mackenzie Delta, to determine if differences in forest structure and organic cover between four common white spruce forest community types were associated with variations in ground temperature. The mean annual temperature at 1‐m depth was lowest (−4.4°C) in the closed/spruce‐feathermoss (CSF) community associated with a thick canopy and thin snow cover, and highest in the recent permafrost of the spruce/alder‐bearberry (SAB) community (−1.0°C) with an open canopy and deep snow. The open‐canopy spruce/crowberry‐lichen (SCL) forest, with a thick surface organic cover and deep snow, had a higher mean annual temperature at 1‐m depth (−2.1°C) than the CSF forest, indicating the importance of canopy cover for snow accumulation and ground heat loss in winter. Seasonal and inter‐annual variation of 4‐m ground temperatures was greatest beneath the CSF community, highlighting the importance of greater winter cooling due to a thin snow cover and a lower unfrozen water content. Temperatures at 20‐m depth ranged from −0.6°C to −1.5°C in SAB forests, and were significantly lower in CSF, open/spruce‐feathermoss and SCL communities (−1.6°C to −2.9°C). Variation in near‐surface temperatures between spruce forest types diminishes with depth due to the thermal influence of water bodies. There was no significant variation of ground temperatures at 20‐m depth within spruce forest communities in different parts of the delta. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada. Article in Journal/Newspaper Crowberry Mackenzie Delta Northwest Territories permafrost Permafrost and Periglacial Processes Wiley Online Library Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Northwest Territories Permafrost and Periglacial Processes 20 2 127 139
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Surface conditions and ground temperatures from 50‐cm to 20‐m depth were measured at 26 forested sites in the Mackenzie Delta, to determine if differences in forest structure and organic cover between four common white spruce forest community types were associated with variations in ground temperature. The mean annual temperature at 1‐m depth was lowest (−4.4°C) in the closed/spruce‐feathermoss (CSF) community associated with a thick canopy and thin snow cover, and highest in the recent permafrost of the spruce/alder‐bearberry (SAB) community (−1.0°C) with an open canopy and deep snow. The open‐canopy spruce/crowberry‐lichen (SCL) forest, with a thick surface organic cover and deep snow, had a higher mean annual temperature at 1‐m depth (−2.1°C) than the CSF forest, indicating the importance of canopy cover for snow accumulation and ground heat loss in winter. Seasonal and inter‐annual variation of 4‐m ground temperatures was greatest beneath the CSF community, highlighting the importance of greater winter cooling due to a thin snow cover and a lower unfrozen water content. Temperatures at 20‐m depth ranged from −0.6°C to −1.5°C in SAB forests, and were significantly lower in CSF, open/spruce‐feathermoss and SCL communities (−1.6°C to −2.9°C). Variation in near‐surface temperatures between spruce forest types diminishes with depth due to the thermal influence of water bodies. There was no significant variation of ground temperatures at 20‐m depth within spruce forest communities in different parts of the delta. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada.
format Article in Journal/Newspaper
author Kanigan, J. C. N.
Burn, C. R.
Kokelj, S. V.
spellingShingle Kanigan, J. C. N.
Burn, C. R.
Kokelj, S. V.
Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
author_facet Kanigan, J. C. N.
Burn, C. R.
Kokelj, S. V.
author_sort Kanigan, J. C. N.
title Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
title_short Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
title_full Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
title_fullStr Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
title_full_unstemmed Ground temperatures in permafrost south of treeline, Mackenzie Delta, Northwest Territories
title_sort ground temperatures in permafrost south of treeline, mackenzie delta, northwest territories
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/ppp.643
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.643
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.643
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Canada
Mackenzie Delta
Northwest Territories
geographic_facet Canada
Mackenzie Delta
Northwest Territories
genre Crowberry
Mackenzie Delta
Northwest Territories
permafrost
Permafrost and Periglacial Processes
genre_facet Crowberry
Mackenzie Delta
Northwest Territories
permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 20, issue 2, page 127-139
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.643
container_title Permafrost and Periglacial Processes
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