This research highlights how climate driven permafrost and thaw slumping is affecting the streams in the Peel Plateau, NWT.

This study analyzes changes in lake area across northwestern Canada (1985–2020) using satellite data, focusing on the influence of climate, wildfire, and permafrost.

In this study we quantify thaw slump enlargement, investigate thermokarst impacts, and map the propagation of effects through hydrological networks draining permafrost terrain.

This paper documents the first comprehensive inventory of thermokarst and thaw-sensitive terrain indicators for a 2 million km2 region of northwestern Canada.