Permafrost‐thaw‐induced land‐cover change in the Canadian subarctic: implications for water resources
- 15 November 2010
- journal article
- scientific briefing
- Published by Wiley in Hydrological Processes
- Vol. 25 (1), 152-158
- https://doi.org/10.1002/hyp.7894
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Arctic Landscapes in Transition: Responses to Thawing PermafrostEos, 2010
- Increasing winter baseflow and mean annual streamflow from possible permafrost thawing in the Northwest Territories, CanadaGeophysical Research Letters, 2009
- Hillslope runoff from an ice‐cored peat plateau in a discontinuous permafrost basin, Northwest Territories, CanadaHydrological Processes, 2008
- A simple heat‐conduction method for simulating the frost‐table depth in hydrological modelsHydrological Processes, 2007
- Evidence and Implications of Recent Climate Change in Northern Alaska and Other Arctic RegionsClimatic Change, 2005
- Permafrost Thaw Accelerates in Boreal Peatlands During Late-20th Century Climate WarmingClimatic Change, 2005
- Hydrologic functions of wetlands in a discontinuous permafrost basin indicated by isotopic and chemical signaturesJournal of Hydrology, 2004
- Connectivity and storage functions of channel fens and flat bogs in northern basinsHydrological Processes, 2003
- Climate and the limits of permafrost: a zonal analysisPermafrost and Periglacial Processes, 2002
- The Influence of Permafrost and Fire upon Carbon Accumulation in High Boreal Peatlands, Northwest Territories, CanadaArctic, Antarctic, and Alpine Research, 2000