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Danger level
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The avalanche danger is low. There is usually not enough snow for snow sports and avalanches can hardly be triggered.
There is no closed snow cover, snowpack and the terrain is mostly bare.
The avalanche danger is rising slightly with the gradual increase in fresh snow and wind on Tuesday, the uncertainty is still high.
Danger level
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The avalanche risk is low, but injury from stones and falling remain the main dangers. In gullies and bowls adjacent to the ridgeline, crests or summits on the shady slopes, there are isolated trigger points in persistent weak layers that are difficult to disturb. In rare cases, drift snow packs can also be triggered there by individuals. Avalanches usually remain small.
The snow cover, snowpack is highly variable. The surface is crusted can form, on sunny slopes it softens during daytime changes. In shady slopes, weak layers of faceted crystals are occasionally preserved in the snow cover, mostly in the vicinity of crusts. Due to the overall heavily built-up transformed snow cover, the fracture propagation potential is generally low. The snow depth is well below average for the time of year.
The avalanche danger is rising slightly with the gradual increase in fresh snow and wind on Tuesday, the uncertainty is still high.
Danger level
| 2600m |
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The avalanche danger is low. Small avalanches in particular can occasionally be triggered by one person in shady slope high alpine regions above 2600 metres. On the one hand, where older wind slab snow has formed a suitable board over a weak layer in the persistent weak layer. On the other hand, close to the surface in the wind slab of the last few days, which is still prone to triggering. Be safe behind ridgelines, in gullies and bowls. In addition to the risk of burial, consideration should be given to the risk of entrainment.
The snow cover, snowpack is highly variable. The surface is crusted can form, on sunny slopes it softens during the daytime changes. In high, shady slopes, the melt-freeze crust is usually covered by edged snow with no binding. The potential for fracture propagation is generally low due to the overall highly built-up, transformed snow cover, snowpack. Fractures are most possible in low thickness wind slab snow, over the hard old snow foundation from early winter, or very rarely in the vicinity of crusts. The snow depth is well below average at all altitudes.
The avalanche danger is rising slightly with the gradual increase in fresh snow and wind on Tuesday, the uncertainty is still high.
