globalchange  > 气候减缓与适应
DOI: 10.1002/2017JF004469
Scopus记录号: 2-s2.0-85042122196
论文题名:
The Influence of Shallow Taliks on Permafrost Thaw and Active Layer Dynamics in Subarctic Canada
作者: Connon R.; Devoie É.; Hayashi M.; Veness T.; Quinton W.
刊名: Journal of Geophysical Research: Earth Surface
ISSN: 21699003
出版年: 2018
卷: 123, 期:2
起始页码: 281
结束页码: 297
语种: 英语
英文关键词: active layer ; peatlands ; permafrost thaw ; suprapermafrost layer ; talik
Scopus关键词: active layer ; freeze-thaw cycle ; heat flux ; peatland ; permafrost ; subarctic region ; talik ; thawing ; Canada
英文摘要: Measurements of active layer thickness (ALT) are typically taken at the end of summer, a time synonymous with maximum thaw depth. By definition, the active layer is the layer above permafrost that freezes and thaws annually. This study, conducted in peatlands of subarctic Canada, in the zone of thawing discontinuous permafrost, demonstrates that the entire thickness of ground atop permafrost does not always refreeze over winter. In these instances, a talik exists between the permafrost and active layer, and ALT must therefore be measured by the depth of refreeze at the end of winter. As talik thickness increases at the expense of the underlying permafrost, ALT is shown to simultaneously decrease. This suggests that the active layer has a maximum thickness that is controlled by the amount of energy lost from the ground to the atmosphere during winter. The taliks documented in this study are relatively thin (<2 m) and exist on forested peat plateaus. The presence of taliks greatly affects the stability of the underlying permafrost. Vertical permafrost thaw was found to be significantly greater in areas with taliks (0.07 m year−1) than without (0.01 m year−1). Furthermore, the spatial distribution of areas with taliks increased between 2011 and 2015 from 20% to 48%, a phenomenon likely caused by an anomalously large ground heat flux input in 2012. Rapid talik development and accelerated permafrost thaw indicates that permafrost loss may exhibit a nonlinear response to warming temperatures. Documentation of refreeze depths and talik development is needed across the circumpolar north. ©2018. American Geophysical Union. All Rights Reserved.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/114496
Appears in Collections:气候减缓与适应

Files in This Item:

There are no files associated with this item.


作者单位: Cold Regions Research Centre, Wilfrid Laurier University, Waterloo, ON, Canada; Department of Civil and Environmental Engineering, University of Waterloo, Waterloo, ON, Canada; Department of Geoscience, University of Calgary, Calgary, AB, Canada

Recommended Citation:
Connon R.,Devoie É.,Hayashi M.,et al. The Influence of Shallow Taliks on Permafrost Thaw and Active Layer Dynamics in Subarctic Canada[J]. Journal of Geophysical Research: Earth Surface,2018-01-01,123(2)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Connon R.]'s Articles
[Devoie É.]'s Articles
[Hayashi M.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Connon R.]'s Articles
[Devoie É.]'s Articles
[Hayashi M.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Connon R.]‘s Articles
[Devoie É.]‘s Articles
[Hayashi M.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.