Avalanche danger above 2000m is moderate, below that altitude danger is low. Main problem: snowdrift accumulations. These can trigger a medium-sized avalanche by one sole skier/snowboarder. Avalanche prone locations occur in steep ridgeline terrain and in wind-loaded gulles and bowls. The snowdrift accumulations are easily recognized for the practiced eye. At lower altitudes the slab avalanche releases are small, larger higher up. Possibility of medium-sized glide-snow avalanches on steep smooth grass-covered slopes in all aspects, releases mostly small, but occasionally medium-sized.
Snowpack
In all aspects, also distant from ridgelines, snowdrift accumulations have been generated, mostly well bonded with the old snowpack surface. But inside the drifts themselves are isolated soft intermediate layers and graupel. The old snowpack base is stable and moist-to-wet at intermediate altitudes. Terrain at intermediate altitudes which is exposed to wind and sun are often bare of snow, only with only a thin covering. In wind-protected terrain there is 10-20 cm of powder.
Tendency
Avalanche danger levels expected to diminish
Danger level
Avalanche Problem
Wind slab
Little snow on the ground
Avalanche danger is low. Main problem: freshly generated snowdrift accumulations which in wind-loaded zones on N/E/S facing slopes can trigger by minimum additional loading. Slab avalanche releases are small, the risks of taking a fall are greater.
Snowpack
Older snowdrifts are generally well bonded with the old snowpack surface but in some areas there are soft intermediate layers and graupel embedded. The old snowpack is generally stable, but moist-to-wet down to the ground. Terrain at intermediate altitudes which is exposed to wind and sun are often bare of snow, only with only a thin covering. In wind-protected terrain there is 10-20 cm of powder.