Seminar Videos – Ice-Wedges of the Hudson Bay Lowlands and Precise Change Detection with Airborne InSAR & Optical Photogrammetry in Active Permafrost Regions.

The NSERC PermafrostNet seminar videos – Ice-Wedge Volume, Distribution, and Development in the Barrens of the Hudson Bay Lowlands, Northern Manitoba and Precise Change Detection with Airborne InSAR and Optical Photogrammetry data in permafrost regions are now available.

Tabatha Rahman presented Ice-Wedge Volume, Distribution, and Development in the Barrens of the Hudson Bay Lowlands, Northern Manitoba.

Extensive ice-wedge polygon networks are found in the ‘Barrens’ of northern Manitoba, a 50,000 km2 zone of continuous permafrost tundra that emerged from the Tyrrell Sea less than 5,500 years ago. Tabatha will present empirical results of ice-wedge volume and tri-dimensional distribution, and will focus on the environmental conditions associated with the growth and degradation of ice wedges in this uplifted permafrost peatland. Knowledge of wedge-ice morphology and development is essential for the prediction and mitigation of risks associated with anticipated permafrost thaw in the Barrens.

Usman Iqbal Ahmed will be presenting Precise Change Detection with Airborne Interferometric Synthetic Aperture Radar (InSAR) & Optical Photogrammetry Data and its application to Active Permafrost Regions.

Permafrost thaw can cause several problems; the ground becomes unstable and can cause damage to infrastructure such as roads, buildings, and pipelines. It can also cause erosion and changes in the landscape, which can have ecological and social impacts and disruption of indigenous ways of life. Monitoring these changes is a key factor in reducing the impact of such disasters as well as timely reaction/adaptation to such changes. I am exploring the option of developing a change detection method using Airborne Synthetic Aperture Radar (SAR) Interferometry and Optical Photogrammetry data for precise change detection. I will present the results of our controlled experiment with simulated permafrost related changes to showcase the capability of our method in active permafrost thaw environments.

Seminar – 15 May – Ice-Wedge Volume, Distribution, and Development in the Barrens of the Hudson Bay Lowlands, Northern Manitoba.

Tabatha Rahman will be presenting Ice-Wedge Volume, Distribution, and Development in the Barrens of the Hudson Bay Lowlands, Northern Manitoba.

Date: 15 May 2024
Time: 13:00-14:00 Eastern Time
Location: Zoom (details are posted in our Teams site).

Extensive ice-wedge polygon networks are found in the ‘Barrens’ of northern Manitoba, a 50,000 km2 zone of continuous permafrost tundra that emerged from the Tyrrell Sea less than 5,500 years ago. Tabatha will present empirical results of ice-wedge volume and tri-dimensional distribution, and will focus on the environmental conditions associated with the growth and degradation of ice wedges in this uplifted permafrost peatland. Knowledge of wedge-ice morphology and development is essential for the prediction and mitigation of risks associated with anticipated permafrost thaw in the Barrens.

Seminar – 8 May – The Effects of Environmental Controls on Epigenetic Ice-Wedge Cracking.

Gabriel Karam will be presenting The Effects of Environmental Controls on Epigenetic Ice-Wedge Cracking.

Date: 8 May 2024
Time: 13:00-14:00 Eastern Time
Location: Zoom (details are posted in our Teams site).

Ice-wedge polygons are a widespread periglacial feature in the continuous permafrost regions. To better understand the mechanical aspects of their formation, the extended finite-element method was employed to simulate the cracking process. Four case studies will be presented, which evaluate the effects different environmental controls and explore the growth of wedges over multiple years.