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Permafrost Thaw Induced Drying of Wetlands at Scotty Creek, NWT, Canada
This article analyzes pernafrost that and long-term water level data to show how wetland drying and landscape changes contribute to shifting hydrology in northern peatland systems. -
Mapping and understanding the Vulnerability of Northern Peatlands to Permafro...
This article is directly focused on the Taiga Plains and discontinuous permafrost zone in the NWT and provides community-scale mapping tools to support land-use planning,... -
NWT Thermokarst Mapping Collective
This project addresses an important knowledge gap on the distribution of thaw-sensitive permafrost terrain across the NWT. -
Ground ice, organic carbon and soluble cations in tundra permafrost soils and...
This study can inform permafrost investigations in other parts of the Slave Geological Province, and its data can support scenario simulations of future trajectories of... -
Long-term Climate-influenced Land Cover Change in Discontinuous Permafrost Pe...
Examines how climate warming and permafrost thaw drive long-term transitions from forested peatlands to wetlands and eventually to permafrost-free forests in northern Canada. -
Particulate Dominance of Organic Carbon Mobilization from Thaw Slumps on the ...
This research highlights how climate driven permafrost and thaw slumping is affecting the streams in the Peel Plateau, NWT. -
Rising Waters: How Streamflow is Increasing in the Southern Taiga Plains
This research helps us understand how climate change, permafrost thaw, and wildfire impact water systems to help predict future changes.
