Page 2: 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.

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 ...

Two Nepalis swept away by Annapurna avalanche

Nepali mountaineers on Tuesday searched for two people swept away by a powerful avalanche on the world's 10th highest mountain Annapurna, officials said.

Gliding avalanches: Field monitoring tackles the great unknowns

In a gliding avalanche, the entire snowpack slides down a suitable substratum such as grass or slabs of rock. Such avalanches are always released naturally. This requires the snow on the ground to become moist. In winter, ...

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