Although landslides occur over a broad range of lithologies, climatologies, hydrological regimes, and land use types (Kirschbaum et al., 2015), the majority are precipitation-triggered (Petley et al., 2005). However, for most precipitation-triggered landslides, other complex atmospheric, surface, and subsurface conditions also play a role in predisposing the slope to failure by increasing the effects of downgradient forces and/or reducing the strength of the underlying slope (Sidle & Ochiai, 2006;Terzaghi, 1950). Isolating the effect of precipitation from these confounding factors is thus essential both for enhancing fundamental understanding of landslides and for evaluating the impact of climate change on slope failure.A principal way that climate change is likely to impact landslide hazard is by intensifying precipitation