Long‐term trends in wetland event response with permafrost thaw‐induced landscape transition and hummock development

Abstract Northwestern Canada's discontinuous permafrost landscape is transitioning rapidly due to permafrost thaw, with the conversion of elevated, forested peat plateaus to low‐lying, treeless wetlands. Increasing hydrological connectivity leads to partial drainage of previously isolated wetla...

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Bibliographic Details
Published in:Ecohydrology
Main Authors: Haynes, Kristine M., Frederick, Ian, Disher, Brenden, Carpino, Olivia, Quinton, William L.
Other Authors: ArcticNet, Natural Sciences and Engineering Research Council of Canada
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2022
Subjects:
Online Access:http://dx.doi.org/10.1002/eco.2515
https://onlinelibrary.wiley.com/doi/pdf/10.1002/eco.2515
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/eco.2515