This study documents erosional processes, recession rates, volume losses, and sediment delivery of Tuktoyaktuk (Tuktuujaqrtuuq) Island since 1947 and projected into the future.

This report provides an inventory of current and old lithalsas in a representative study area between Behchoko and Yellowknife (Sǫ̀mbak'è) in the Northwest Territories.

This report presents results from the first regional-scale approach to map permafrost-related landforms in the Slave Geological Province.

This poster presents permafrost terrain mapping of the Grays Bay - Yellowknife Corridor.

Wilfrid Laurier University researchers created and tested a new method to map land cover types – such as forests, bogs and fens – in the headwaters of the Scotty Creek basin.

Remote sensing is used to derive the annual minimum snow and ice extent over the Canadian Arctic landmass from 2000-2016.

A historical analysis of coastal erosion with the help of photo data.

Ground temperatures were monitored to examine evidence of ground temperature warming and to assess the influence of various environmental factors on permafrost conditions.

Meteorological data used to determine trends and changes in autumn rainfall and winter air temperatures over a 37-year record, and streamflow was used to calculate the total...

This research looked at how the yearly snowpack is changing, and how it may influence the well-being of the Bathurst caribou herd.

To help understand the impact of changes to caribou habitat their decline, we analyzed satellite imagery to detect changes in vegetation in the Bathurst caribou herd range.

The NWT Thermokarst Mapping Collective project developed a methodology to generate NWT-wide thermokarst and permafrost feature inventory maps.

Using aerial imagery and ground survey data from Pullen Island, NWT, we observe increasing coastal erosion rates between 1947 to 2018.

This study furthers the geomorphological understanding of RTS processes along Arctic coasts, and demonstrates advancements in measurement practices for UAV-SfM data.

This paper shows that climate-driven thaw of hilltop ice-wedge networks is rapidly transforming uplands across Banks Island in the Canadian Arctic Archipelago.

Active layer thickness data paired with Landsat data were used to quantify the impacts of changing permafrost conditions on vegetation productivity in the NWT.