Landslide and debris flow response to past and present climate change in the Canadian Arctic

Arctic landscapes are among the most vulnerable on Earth to climate change, largely due to the rapid degradation of permafrost. In steeper bedrock-dominated terrains, warming permafrost can lead to increased sediment production via mass wasting events and amplify the delivery of sediment to channels and lakes. However, there is a fundamental lack of data on current rates of sediment production and transport in Arctic watersheds, especially those still responding to post-glacial perturbations, making it impossible to predict the responses and rates of sediment transport processes under future climate change. In this talk, I will present findings from a field-based study of the Black Mountain catchment in the Aklavik Range (Canada). This site was chosen due to the presence of an alluvial fan that post-dates the retreat of the Laurentide Ice Sheet (LIS), providing a closed system where we can consider how both paraglacial and periglacial mass flow processes have influenced physical weathering and transport rates through time.