Papers and Presentations

Limber Pine Seed and Seedling Planting Experiment
November 25, 2011
Integrating Physical and Empirical Landslide Susceptibility Models Using Generalized Additive Models
May 1, 2011
Extreme Weather and Landslide Initiation in Coastal British Columbia
March 14, 2011
Environmental factors associated with reproductive barrier breakdown in sympatric trout populations on Vancouver Island
March 14, 2011
Integrating Physical and Empirical Landslide Susceptibility Models Using Generalized Additive Models
March 10, 2011

Limber pine plays an important role in the harsh environments in which it lives, providing numerous ecological services, especially because its large, wingless seeds serve as a high energy food source for many animals. Limber pine populations are declining due to a combination of white pine blister rust, mountain pine beetle, drought, and fire suppression. Outplanting of seedlings is a common strategy to aid in restoration efforts, but the success of revegetation methods in limber pine habitats is little known. To aid in restoration efforts in Waterton Lakes National Park, in southwestern Alberta, and other impacted areas, we studied the survival of limber pine planted as seeds and those planted as seedlings. At our experimental site, 11 percent of the seeds had germinated and seedlings were still alive after three years, while 72 percent of the seedlings that were planted directly survived. Restoration efforts are likely to have greater success when limber pine is planted in groups of five as seedlings rather than as seeds and there may be benefit to planting seedlings in burned areas near cover such as rocks or stumps.

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Physically based models are commonly used as an integral step in landslide hazard assessment. Geomorphic principles can be applied to a broad area, resulting in first order assessment of landslide susceptibility. New techniques are now available that may result in the increased accuracy of such models. We investigate the possibility to enhance landslide susceptibility modeling by integrating two physically-based landslide models, the Factor of Safety (FS) and the Shallow Stability model (SHALSTAB), with traditional empirical–statistical methods that utilize terrain attribute information derived from a digital elevation model and land use characteristics related to forest harvesting. The model performance is measured by the area under the receiver operating characteristic curve (AUROC) and sensitivity at 90% and 80% specificity both estimated by bootstrap resampling. Our study examines 278 landslide initiation points in the Klanawa Watershed located on Vancouver Island, British Columbia, Canada. We use a generalized additive model (GAM) and a logistic regression model (GLM) combining physical landslide models, terrain attributes and land use data, and GAMs and GLMs using only subsets of these variables. In this study, all empirical and combined physical–empirical models outperform the physically-based models, with GAMs often performing significantly better than GLMs. The strongest predictive performance is achieved by the GAMs using terrain attributes in combination with land use data. Variables representing physically-based models do not significantly improve the empirical models, but they may allow for a better physical interpretation of empirical models. Also, based on bootstrap variable-selection frequencies, land use data, FS, slope and plan/profile curvature are relatively the most important predictor variables.

More frequent more intense storms predicted by climate models for the Pacific Northwest of North America could increase the regional landslide hazard. The impacts of one such storm are examined on Vancouver Island, British Columbia, during which 626 mapped landslides occurred, encompassing >5 km2 total area and generating >1.5 × 106 m3 of sediment. The relationship between rainfall intensity, air temperature and wind speed obtained from mesoscale numerical weather modelling is examined relative to landslide incidence within steep terrain. A critical onset of rainfall intensity between 80 and 100 mm in 24 h that results in a rapid increase in landslides with increasing precipitation is demonstrated. The argument is presented that this result is more useful for landslide management decisions than a minimum threshold. The component of wind-driven rain was calculated, and results indicated that wind caused increased concentrations of rainfall associated with the occurrence of landslides.

Approximately half the landslides studied were not related to rainfall alone, but to rain on snow, and we argue that wind played a crucial role. This often neglected component of hydrological analysis remains a major challenge as the role of snow transition zones and a warming climate in coastal mountain watersheds is considered.

Over the last several years, Cory Bettles has published a number of peer-reviewed publications and professional reports related to fisheries conservation and management. Most recently, he published a manuscript in the international Journal Evolutionary Applications that investigated the environmental indicators associated with reproductive barrier breakdown (hybridization) in two trout species on Vancouver Island, BC.

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We investigate the possibility to enhance landslide susceptibility modeling by integrating two physically-based landslide models, the Factor of Safety (FS) and the Shallow Stability model (SHALSTAB). In this study, all empirical and combined physical–empirical models outperform the physically-based models.

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