Results 31 to 40 of about 32,126 (216)

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

open access: yesJournal of Geophysical Research: 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
Wever, Nander   +2 more
openaire   +1 more source

Distributed snow and rock temperature modelling in steep rock walls using Alpine3D [PDF]

open access: yesThe Cryosphere, 2017
In this study we modelled the influence of the spatially and temporally heterogeneous snow cover on the surface energy balance and thus on rock temperatures in two rugged, steep rock walls on the Gemsstock ridge in the central Swiss Alps.
A. Haberkorn   +6 more
doaj   +1 more source

Soil erosion and organic carbon export by wet snow avalanches [PDF]

open access: yes, 2014
Many mountain belts sustain prolonged snow cover for parts of the year, although enquiries into rates of erosion in these landscapes have focused almost exclusively on the snow-free periods.
C. Rixen, O. Korup
core   +1 more source

Scaling precipitation input to spatially distributed hydrological models by measured snow distribution

open access: yesFrontiers in Earth Science, 2016
Accurate knowledge on snow distribution in alpine terrain is crucial for various applicationssuch as flood risk assessment, avalanche warning or managing water supply and hydro-power.To simulate the seasonal snow cover development in alpine terrain, the ...
Christian Vögeli   +5 more
doaj   +1 more source

Influence of stress, temperature and crystal morphology on isothermal densification and specific surface area decrease of new snow [PDF]

open access: yesThe Cryosphere, 2014
Laboratory-based, experimental data for the microstructural evolution of new snow are scarce, though applications would benefit from a quantitative characterization of the main influences.
S. Schleef, H. Löwe, M. Schneebeli
doaj   +1 more source

A new experimental snow avalanche test site at Seehore peak in Aosta Valley (NW Italian Alps) - Part II: Engineering aspects [PDF]

open access: yes, 2013
The estimate of the effects produced by the impact of a snow avalanche against an obstacle is of the utmost importance in designing safe mountain constructions.
Ammann   +26 more
core   +2 more sources

A methodology to allow avalanche forecasting on an information retrieval system [PDF]

open access: yes, 1998
This paper presents adaptations and tests undertaken to allow an information retrieval (IR) system to forecast the likelihood of avalanches on a particular day.
Buser O   +8 more
core   +1 more source

Automated snow avalanche release area delineation – validation of existing algorithms and proposition of a new object-based approach for large-scale hazard indication mapping [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2018
Snow avalanche hazard is threatening people and infrastructure in all alpine regions with seasonal or permanent snow cover around the globe. Coping with this hazard is a big challenge and during the past centuries, different strategies were developed.
Y. Bühler   +6 more
doaj   +1 more source

Snow in a very steep rock face: accumulation and redistribution during and after a snowfall event

open access: yesFrontiers in Earth Science, 2015
Terrestrial laser scanning was used to measure snow thickness changes (perpendicular to the surface) in a rock face. The aim was to investigate the accumulation and redistribution of snow in extremely steep terrain (>60°).
Christian Gabriel Sommer   +4 more
doaj   +1 more source

A Comparison of Frequency Domain Electro-Magnetometry, Electrical Resistivity Tomography and Borehole Temperatures to Assess the Presence of Ice in a Rock Glacier

open access: yesFrontiers in Earth Science, 2020
Alpine permafrost is currently warming, leading to changes such as active layer deepening and talik formation. Frequency domain electro-magnetometry (FDEM) measurements were tested as a simple and efficient method to investigate ground characteristics ...
Jacopo Boaga   +6 more
doaj   +1 more source

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