Thesis Defence: River morphodynamic response in a watershed affected by megafires (Deadman River, British Columbia, Canada)

Gareth J. T. Wells, supervised by Dr. Alessandro Ielpi, will defend their thesis titled “River morphodynamic response in a watershed affected by megafires (Deadman River, British Columbia, Canada)” in partial fulfillment of the requirements for the degree of Master of Science in Earth and Environmental Sciences.

An abstract for Gareth J. T. Wells’ thesis is included below.

Defences are open to all members of the campus community as well as the general public. Registration is not required for in-person defences.

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Abstract

Wildfires can have profound impacts on the movement of water and sediment along watersheds due primarily to changes in the mechanical and hydrologic properties of vegetation and soil. Previous studies have documented the damaging dynamics of local post-wildfire landslides, debris floods and flows, though little attention has been paid to larger watershed-scale fluvial responses. To address this knowledge gap, this study focuses on the Deadman River watershed, which was severely affected by the Elephant Hill and Sparks Lake fires of, respectively, 2017 and 2021 in the southern interior of British Columbia, Canada. We included results from field-data collection, multispectral remote sensing, and timelapse photogrammetry, to examine how fire-related changes in hydrology and sediment flux have influenced channel morphology and meander migration. The timelapse imagery analysis indicates a broad, watershed-wide increase in channel width and meander migration rate over the observed timespan (2002–2023), with a sharp increase in these metrics (up to 100% and 540%, respectively) in the aftermath of the 2021 fire. Integration of sub-catchment-scale burn severity analysis reveals that regions that burned more severely drained into reaches that migrated laterally at faster rates. We observed a dependency of channel migration rate on integration timescale that was primarily attributed to channel-migration reversals and chute cutoffs. We finally conducted a normalization of migration rate to demonstrate that the observed post-fire morphodynamic changes are not an artifact of integration timescale – a conclusion corroborated by the relationships with channel width, which is not sensitive to integration timescale. These results provide a quantification of the degree to which wildfires can alter the morphodynamics of meandering rivers and their catchments. We anticipate our study to inform natural hazard mitigation efforts as well as longer-term ecosystem restoration and recovery efforts in area affected by megafires.