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.

Nepal flood disaster exposes cascading threats in Himalayas

A catastrophic flood in Nepal that left thousands missing began with a collapse of ice and rock high in the mountains—a warning that disaster planning must prepare for chains of hazards, not isolated events, experts say.

Nepal floods highlight growing glacier risks in warming Himalayas

The deadly flash flood in Nepal on Wednesday was likely caused by a huge chunk of a glacier that broke off and temporarily dammed a river, according to preliminary investigations by scientists. That may have led to the backed-up ...

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