Results 21 to 30 of about 186,325 (230)
Initial snow-ice formation on a laboratory scale
Snow ice (SI) forms from freezing wet snow, known as slush, and contributes to the thickness of level and brash ice. However, the mechanism of snow-slush-snow ice transformation has not been extensively investigated to date, despite the difference in the
Vasiola Zhaka +4 more
doaj +1 more source
Looking beyond the powder/dense flow avalanche dichotomy [PDF]
Köhler et al. (2018) deploy a high spatial and temporal resolution GEODAR radar system to reveal the inside of snow avalanches over the entire slope.
Faug, T., Gauer, P., Turnbull, Barbara
core +4 more sources
Full snow-pit observations were performed on a monthly basis over ten winter seasons from 1995 to 2004, at 15 study plots spaced at 100 m elevation intervals (1300–2700 m a.s.l.) in the mountainous forest of the Japanese Central Alps.
Yusuke Harada +2 more
doaj +1 more source
Modelling the transition from grain-boundary sliding to power-law creep in dry snow densification
This paper presents a physics-based macroscale model for the densification of dry snow which provides for a smooth transition between densification by grain-boundary sliding (stage 1) and densification by power-law creep (stage 2).
Elizabeth M. Morris +2 more
doaj +1 more source
Macroscopic water vapor diffusion is not enhanced in snow [PDF]
Water vapor transport in dry snowpacks plays a significant role for snow metamorphism and the mass and energy balance of snowpacks. The molecular diffusion of water vapor in the interstitial pores is usually considered to be the main or only transport ...
K. Fourteau +3 more
doaj +1 more source
Comparing measurements of snow mechanical properties relevant for slab avalanche release
Snow properties relevant to the fracture processes involved in dry-snow slab avalanche release include weak layer specific fracture energy, slab elastic modulus and density.
BENJAMIN REUTER +4 more
doaj +1 more source
Modeling the small-scale deposition of snow onto structured Arctic sea ice during a MOSAiC storm using snowBedFoam 1.0. [PDF]
The remoteness and extreme conditions of the Arctic make it a very difficult environment to investigate. In these polar regions covered by sea ice, the wind is relatively strong due to the absence of obstructions and redistributes a large part of the ...
O. Hames +13 more
doaj +1 more source
Owing to drifting snow processes, snow accumulation and surface density in polar environments are variable in space and time. We present new field data of manual measurements, repeat terrestrial laser scanning and snow micro-penetrometry from Dronning ...
Nander Wever +6 more
doaj +1 more source
Decoupling of a Neutron Interferometer from Temperature Gradients [PDF]
Neutron interferometry enables precision measurements that are typically operated within elaborate, multi-layered facilities which provide substantial shielding from environmental noise.
A. R. Young +16 more
core +2 more sources
Abstract. Seasonal snow is an essential component of regional and global water and energy cycles, particularly in snow-dominant regions that rely on snowmelt for water resources. Land surface models (LSMs) are a common approach for developing spatially and temporally complete estimates of snow water equivalent (SWE) and hydrologic variables at a large ...
E. Cho +9 more
openaire +3 more sources

