Results 11 to 20 of about 2,059 (159)

Snow mechanics

open access: yesEos, Transactions American Geophysical Union, 1974
The International Symposium on Snow Mechanics was held April 1–5, 1974, in Grindelwald, Switzerland, under the sponsorship of the International Association of Hydrological Science.The conference, organized by the International Commission on Snow and Ice, attracted participants from a number of countries to discuss the physical and mechanical ...
Samuel C. Colbeck, R. I. Perla
openaire   +1 more source

Probabilistic size effect law for mode II fracture from critical lengths in snow slab avalanche weak layers

open access: yesJournal of Glaciology, 2019
From field observations, dry snow slab avalanche initiation is associated with fracture within relatively thin weak layers under stronger, cohesive slabs.
D. M. McCLUNG, C. P. BORSTAD
doaj   +1 more source

Angle of repose experiments with snow: role of grain shape and cohesion

open access: yesJournal of Glaciology, 2020
Snow appears as a granular material in most engineering applications. We examined the role of grain shape and cohesion in angle of repose experiments, which are a common means for the characterization of granular materials. The role of shape was examined
Carolin Willibald   +4 more
doaj   +1 more source

Detrainment and braking of snow avalanches interacting with forests [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2022
Mountain forests provide natural protection against avalanches. They can both prevent avalanche formation in release zones and reduce avalanche mobility in runout areas.
L. Védrine   +4 more
doaj   +1 more source

Heterogeneous grain growth and vertical mass transfer within a snow layer under a temperature gradient [PDF]

open access: yesThe Cryosphere, 2023
Inside a snow cover, metamorphism plays a key role in snow evolution at different scales. This study focuses on the impact of temperature gradient metamorphism on a snow layer in its vertical extent.
L. Bouvet   +4 more
doaj   +1 more source

Snow-Collection Mechanisms and the Capacities of Snow Fences [PDF]

open access: yesAnnals of Glaciology, 1989
The shapes of equilibrium lee drifts formed by snow fences are scaled in proportion to height of snow fences independent of the snow and weather conditions, even in small-scale models, but those of up-wind drifts are not.Field studies have been made of the snow-collection mechanisms of a snow fence.
openaire   +1 more source

Avalanche dynamics by Newton. Reply to comments on avalanche flow models based on the concept of random kinetic energy

open access: yesJournal of Glaciology, 2018
The critique by Issler and other (2017) of our avalanche dynamics model maintains that we disregard well-established results of particulate gravity flows.
PERRY BARTELT, OTHMAR BUSER
doaj   +1 more source

Wind conditions for snow cornice formation in a wind tunnel [PDF]

open access: yesThe Cryosphere, 2023
Snow cornices growing on the leeward side of mountain ridges are common in alpine and polar regions during snow seasons. These structures may crack and fall, leading to an increase in avalanche danger. Although cornice formation has been observed in wind
H. Yu   +8 more
doaj   +1 more source

Mechanism and effects of snow accumulations and controls by lightweight snow fences [PDF]

open access: yesJournal of Modern Transportation, 2016
This paper investigates the snowdrifts caused by lightweight fences along the lines on the flatland through the computational fluid dynamics method. The characteristic ambient flows around the solid fences and the porous fences with varied heights and bottom wind gaps are simulated in the numerical model, and the working mechanism of “interception” and
Liu, Duote   +4 more
openaire   +1 more source

Acoustic emission signatures prior to snow failure

open access: yesJournal of Glaciology, 2018
Snow slab avalanches are caused by cracks forming and propagating in a weak snow layer below a cohesive slab. The gradual damage process leading to the formation of the initial failure within the weak layer (WL) is still not entirely understood.
ACHILLE CAPELLI   +2 more
doaj   +1 more source

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