Research news on avalanche

An avalanche is a rapid, gravity-driven flow of snow, ice, and often entrained rock and debris that propagates downslope once the shear stress within a snowpack exceeds its shear strength. It emerges from mechanical instabilities in stratified snow layers, commonly at interfaces between weak layers and overlying cohesive slabs, triggered by loading, temperature gradients, or external perturbations. Avalanches can exhibit distinct flow regimes, including slab avalanches with brittle fracture and propagating crack fronts, loose-snow avalanches with point-release dynamics, and powder-snow avalanches characterized by turbulent, dilute suspensions. Their behavior is studied using snow mechanics, rheology, and fluid dynamics to model initiation, propagation, and runout.

Cracks in snow propagate faster than expected

Since 10 January 2026, the WSL Institute for Snow and Avalanche Research (SLF) has received reports of hundreds of "whumpfs" (i.e., sounds indicating a collapse in the snowpack) and of remote triggering events—unmistakable ...

Snow's compressibility acts as avalanche crumple zone

How do avalanches affect pylons and other sensitive infrastructure? Using detailed simulations, SLF researcher Michael Kohler has shown that the compressibility of snow initially reduces avalanche pressure, but that at high ...

Avalanches are of key importance to glaciers worldwide

An international research team has shown that avalanches are crucial to the survival of many glaciers worldwide. The study aims to contribute to better predictions of water resources and natural hazards in the context of ...

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