The hydrology of interconnected bog complexes in discontinuous permafrost terrains-Reference-Cited by-同舟云学术

The hydrology of interconnected bog complexes in discontinuous permafrost terrains

Published:2015-07-29 Issue:18 Volume:29 Page:3831-3847
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Connon R. F.¹,Quinton W. L.¹,Craig J. R.²,Hanisch J.³,Sonnentag O.³

Affiliation:

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

2. Department of Civil and Environmental Engineering; University of Waterloo; Waterloo ON Canada

3. Département de géographie; Université de Montréal; Montréal QC Canada

Funder

Canadian Space Agency

Natural Sciences and Engineering Research Council of Canada

W. Garfield Weston Foundation

Publisher

Wiley

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/hyp.10604/fullpdf

Reference49 articles.

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

2. Forests on thawing permafrost: fragmentation, edge effects, and net forest loss;Baltzer;Global Change Biology,2014

3. Changes in forest productivity across Alaska consistent with biome shift;Beck;Ecology Letters,2011

4. An overview of temporary stream hydrology in Canada;Buttle;Canadian Water Resources Journal,2012

5. Quantifying errors in discontinuous permafrost plateau change from optical data, Northwest Territories, Canada : 1947 - 2008;Chasmer;Canadian Journal of Remote Sensing,2011

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