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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,... -
Fort Good Hope (Rádeyı̨lı̨ Kǫ́) 200-year Ice Jam Flood Hazard Map – Climate C...
200-year Ice Jam Flood Hazard Map – Climate Change Scenario 2040-2065 for the Fort Good Hope (Rádeyı̨lı̨ Kǫ́). -
Fort Good Hope (Rádeyı̨lı̨ Kǫ́) 100-year Ice Jam Flood Hazard Map – Climate C...
100-year Ice Jam Flood Hazard Map – Climate Change Scenario 2040-2065 for the Fort Good Hope (Rádeyı̨lı̨ Kǫ́). -
Fort Good Hope (Rádeyı̨lı̨ Kǫ́) 100-year Ice Jam Flood Hazard Map – 1:3000 sc...
100-Year Ice Jam Flood Hazard Maps for Fort Good Hope (Rádęyį̨lį̨ Kóę́). -
Fort Good Hope (Rádeyı̨lı̨ Kǫ́) 200-year Ice Jam Flood Hazard Map – 1:3000 sc...
200-Year Ice Jam Hazard Maps for Fort Good Hope (Rádęyį̨lį̨ Kóę́). -
Fort Good Hope (Rádeyı̨lı̨ Kǫ́) 2021 Flood Inundation Map - 1:3000 scale and ...
May 2021 Ice Jam Flood Inundation Maps for Fort Good Hope (Rádęyį̨lį̨ Kóę́) -
Fort Good Hope (Rádęyį̨lį̨ Kóę́) Flood Study – Final Report 2026
These reports summarizes the results for the new flood study for Fort Good Hope (Rádęyį̨lį̨ Kóę́). -
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... -
Interannual Variability in Air Temperature and Snow Drives Differences in Ice...
This study investigates how interannual variability in air temperature and snowfall influences lake ice formation, freeze-up timing, and ice growth in a subarctic lake near... -
Fort Good Hope (Rádęyį̨lį̨ Kóę́) Flood Study – Final Report Appendix G
This is an 100-Year Flood Inundation Map (Climate Change 2040-2065) for Fort Good Hope (Rádęyį̨lį̨ Kóę́). -
Modeling Emissions Reductions Pathways in the Northwest Territories
This report uses energy-economy modeling to examine greenhouse gas emissions in the Northwest Territories and assess pathways to meet 2030 and net zero 2050 targets. -
Knowledge Agenda: Northern Research for Northern Priorities
The Knowledge Agenda: Northern Research for Northern Priorities 2025 outlines the research priorities of the Government of the Northwest Territories (GNWT). -
2024 NWT Climate Change Risks and Opportunities Assessment
This first NWT Climate Change Risks and Opportunities Assessment, published in October 2024, aims to provide a shared understanding of the most pressing climate change risks for... -
Threats to Biodiversity - Climate Change
This resource provides long-term water quality monitoring data that can help identify climate-driven environmental changes in northern freshwater systems. -
2024 Northwest Territories State of the Conservation Network Report
The report is to provide an update on the state of the conservation network in the Northwest Territories (NWT) . -
Four Decades of Lake Surface Temperature in the NT Using a Lake-Specific Sate...
This study analyzed lake surface temperature trends and spatial distribution across 535 predominantly small to medium lakes across the North Slave Region. -
Effects of Nitrogen and Phosphorus Amendments on CO2 andCH4 Production in Pea...
This study shows how permafrost thaw, wildfires, and added nutrients can increase CO₂ and methane emissions from northern peatlands, affecting carbon cycling. -
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.