Lateral downslope flow in snow during snowmelt and rain‐on‐snow (ROS) events is a well‐
known phenomenon, yet its relevance to water redistribution at hillslope and catchment …

Deep persistent slab avalanches are capable of destroying infrastructure and are usually
unsurvivable for those who are caught. Formation of a snowpack conducive to deep …

Slushflows, defined as rapid mass-movements of water-saturated snow, occur when high
liquid water content (LWC) causes bonds to melt and the snowpack to lose cohesion …

Wet snow avalanches pose a problem for annual spring road opening operations along the
Going-to-the-Sun Road (GTSR) in Glacier National Park, Montana, USA. A suite of …

Understanding the mechanisms by which catchments route vertical water inputs laterally to
stream channels is central to the development of accurate predictive models of watershed …

Deep persistent slab avalanches are a natural hazard that are particularly difficult to predict.
These avalanches are capable of destroying infrastructure in mountain settings, and are …

Nonpersistent snow crystals are deposited during storms, last for a few days, and are
common fracture planes in avalanches. Because avalanches on persistent crystals cause …