Abstract
A destructive debris flood occurred between 19 and 21 June 2013 on Cougar Creek, located in Canmore, Alberta. Cougar Creek fan is likely the most densely developed alluvial fan in Canada. While no lives were lost, the event resulted in approximately $40 M of damage and closed both the Trans-Canada Highway (Highway 1) and the Canadian Pacific Railway line for a period of several days. The debris flood triggered a comprehensive hazard assessment which is the focus of this paper. Debris-flood frequencies and magnitudes are determined by combining several quantitative methods including photogrammetry, dendrochronology, radiometric dating, test pit logging, empirical relationships between rainfall volumes and sediment volumes, and landslide dam outburst flood modeling. The data analysis suggests that three distinct process types act in the watershed. The most frequent process is normal or “clearwater” floods. Less frequent but more damaging are debris floods during which excessive amounts of bedload are transported on the fan, typically associated with rapid and extensive bank erosion and channel infilling and widening. The third and most destructive process is interpreted to be landslide dam outbreak floods. This event type is estimated to occur at return periods exceeding 300 years. Using a cumulative magnitude frequency technique, the data for conventional debris floods were plotted up to the 100–300s year return period. A peak-over-threshold approach was used for landslide dam outbreak floods occurring at return periods exceeding 300 years, as not all such events were identified during test trenching. Hydrographs for 6 return period classes were approximated by using the estimated peak discharges and fitting the hydrograph shape to integrate to the debris flood volumes as determined from the frequency-magnitude relationship. The fan volume was calculated and compared with the integrated frequency-magnitude curve to check of the validity of the latter. A reasonable match was accomplished, verifying the overall relationship. The findings from this work were later used as input to a risk assessment seeking to quantify risk to loss of life and economic losses. The risk assessment then formed the basis for design of debris-flood mitigation structures.
Highlights
The southwestern Alberta mountain front was affected by a high intensity/duration rainstorm between 19 and 21 June 2013
Based on the field investigations, it was determined that debris floods on Cougar Creek are triggered by two processes that may interact to some degree: intensive rainfall events and landslide dam outbreak floods
The second data population is interpreted to consist of debris floods triggered by hillslope processes feeding sediment to the main channel as well as landslide dam outbreaks from either tributary debris-flows or rock slides of variable size
Summary
The southwestern Alberta mountain front was affected by a high intensity/duration rainstorm between 19 and 21 June 2013. Direct runoff, coupled with meltwater released from rain on a shallow snowpack, caused sudden and prolonged high flows in the Bow, High, and Ghost Rivers and their. Hydrology 2017, 4, 7 tributaries originating in the Rocky Mountains. These flows resulted in high rates and volumes of sediment transport, bank erosion and avulsions on alluvial fans. Almost all of the steep gradient tributaries to Bow River within the municipal boundary of the. Town of Canmore were affected by the combined storm andthe snowmelt runoff, including Cougar. Almost all of(Town) the steep gradient tributaries to Bow River within municipal boundary of the Town Creek (Figure 1). Creek fan due to sediment deposition and of Canmore (Town) were affected by the combined storm and snowmelt runoff, including Cougar Creek bank erosion alongdamage the principal channel flanked development
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