Results 1 to 10 of about 1,870 (182)

Signatures of the sub-Rayleigh to supershear fracture transition in snow avalanche experiments [PDF]

open access: yesNature Communications
Snow slab avalanches occur when a crack propagates within a highly porous weak snow layer buried beneath a cohesive snow slab. Here, we report direct observations of a supershear event in snow fracture experiments following the spontaneous transition ...
Bastian Bergfeld   +5 more
doaj   +2 more sources

Snow avalanche formation [PDF]

open access: yesReviews of Geophysics, 2003
Snow avalanches are a major natural hazard, endangering human life and infrastructure in mountainous areas throughout the world. In many countries with seasonally snow‐covered mountains, avalanche‐forecasting services reliably warn the public by issuing occurrence probabilities for a certain region.
Jürg Schweizer, Martin Schneebeli
exaly   +2 more sources

River temperature response to atmospheric heatwaves is modulated by discharge and meltwater [PDF]

open access: yesCommunications Earth & Environment
Alpine rivers are becoming increasingly exposed to atmospheric heatwaves. Because of their strong relationship with air temperature, rivers can experience persistent heat anomalies, known as riverine heatwaves, which can have serious consequences for ...
Amber van Hamel   +2 more
doaj   +2 more sources

Coupled Snow Cover and Avalanche Dynamics Simulations to Evaluate Wet Snow Avalanche Activity [PDF]

open access: yesJournal of Geophysical Research F: Earth Surface, 2018
We present physics‐based snowpack simulations for four snow seasons with detailed wet snow avalanche activity records. The distributed, spatially explicit simulations using the Alpine3D and SNOWPACK model show that the simulated snowpack in the release areas of documented wet snow avalanches often exhibits its first wetting of the season on the release
Nander Wever   +2 more
exaly   +3 more sources

Climate warming enhances snow avalanche risk in the Western Himalayas [PDF]

open access: yesProceedings of the National Academy of Sciences of the United States of America, 2018
J A Ballesteros-Cánovas   +2 more
exaly   +2 more sources

Photogrammetrically UAV based terrain data generation and automatic extraction of torrential properties [PDF]

open access: yesE3S Web of Conferences, 2023
Debris flows are a severe hazard in mountainous regions. However, cost-effective long-term studies of debris flows are seldom, which leads to substantial uncertainties in hazard mitigation methods.
Schmucki Gregor Rafael   +7 more
doaj   +1 more source

Multi-component avalanches for rock- and ice-falls to potential debris flow transition modelling [PDF]

open access: yesE3S Web of Conferences, 2023
Rock/ice avalanches are complex gravitational flows involving three important physicalprocesses: entrainment, phase-changes, and flow transitions. The basic complexity of modelling rock/ice avalanches lies in the fact that the flow is a mixture of rock ...
Munch Jessica   +2 more
doaj   +1 more source

Micromechanical modeling of snow failure [PDF]

open access: yesThe Cryosphere, 2020
Dry-snow slab avalanches start with the formation of a local failure in a highly porous weak layer underlying a cohesive snow slab. If followed by rapid crack propagation within the weak layer and finally a tensile fracture through the slab, a slab ...
G. Bobillier   +7 more
doaj   +1 more source

The RHOSSA campaign: multi-resolution monitoring of the seasonal evolution of the structure and mechanical stability of an alpine snowpack [PDF]

open access: yesThe Cryosphere, 2020
The necessity of characterizing snow through objective, physically motivated parameters has led to new model formulations and new measurement techniques.
N. Calonne   +9 more
doaj   +1 more source

Prediction of natural dry-snow avalanche activity using physics-based snowpack simulations [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2023
Predicting the timing and size of natural snow avalanches is crucial for local and regional decision makers but remains one of the major challenges in avalanche forecasting.
S. Mayer   +3 more
doaj   +1 more source

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