Changing hydrologic connectivity due to permafrost thaw in the lower Liard River valley, NWT, Canada-Reference-Cited by-同舟云学术

Changing hydrologic connectivity due to permafrost thaw in the lower Liard River valley, NWT, Canada

Published:2014-05-18 Issue:14 Volume:28 Page:4163-4178
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Connon Ryan F.¹,Quinton William L.¹,Craig James R.²,Hayashi Masaki³

Affiliation:

1. Centre for Cold Regions and Water Science; Wilfrid Laurier University; Waterloo Ontario Canada

2. Department of Environmental Engineering; University of Waterloo; Waterloo Ontario Canada

3. Department of Geology and Geophysics; University of Calgary; Calgary Alberta Canada

Funder

Canadian Space Agency

Canadian Foundation for Climate and Atmospheric Sciences

Publisher

Wiley

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/hyp.10206/fullpdf

Reference36 articles.

1. Distribution of Fen and Bog in the Mackenzie Valley, 60°N-60°N. Natural Resources Canada;Aylesworth;Geological Survey of Canada Bulletin,2000

2. Beilman DW Robinson SD 2003 Peatland permafrost thaw and landform type along a climate gradient Proceedings of the Permafrost Eighth International Conference 1 61 65

3. Shallow ground temperatures. Natural Resources Canada;Burgess;Geological Survey of Canada Bulletin,2000

4. Inferring groundwater contributions and pathways to streamflow during snowmelt over multiple years in a discontinuous permafrost subarctic environment (Yukon, Canada);Carey;Hydrogeology Journal,2012

5. Quantifying errors in discontinuous permafrost plateau change from optical data, Northwest Territories, Canada; 1947-2008;Chasmer;Canadian Journal of Remote Sensing,2010

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