Hydrological feedbacks in northern peatlands

Author:

Waddington J. M.1,Morris P. J.2,Kettridge N.3,Granath G.14,Thompson D. K.5,Moore P. A.1

Affiliation:

1. School of Geography and Earth Sciences; McMaster University; Hamilton Ontario L8S 4 K1 Canada

2. School of Geography; University of Leeds; Leeds LS2 9JT UK

3. School of Geography, Earth and Environmental Sciences; University of Birmingham; Birmingham B15 2TT UK

4. Department of Aquatic Sciences and Assessment; Swedish University of Agricultural Sciences; SE-750 07 Uppsala Sweden

5. Natural Resources Canada, Canadian Forest Service; Northern Forestry Centre; Edmonton Alberta T6H 3S5 Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Wiley

Subject

Earth-Surface Processes,Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics

Reference155 articles.

1. Partitioning of latent heat flux at a northern peatland;Admiral;Aquatic Botany,2007

2. Size-mediated tree transpiration along soil drainage gradients in a boreal black spruce forest wildfire chronosequence;Angstmann;Tree Physiology,2012

3. A partial explanation of the dependency of hydraulic conductivity on positive pore water pressure in peat soils;Baird;Earth Surface Processes Landforms,1995

4. The DigiBog model of peatland development 1: rationale, conceptual model, and hydrological basis;Baird;Ecohydrology,2012

5. Baisley SA 2012 Effect of drying induce afforestation on peatland ecohydrology: implications for wildfire vulnerability

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