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Avalanche danger is low. Wet snow can be problematic. On extremely steep sunny slopes, isolated small loose-snow avalanches can trigger naturally. In isolated cases, small, older snowdrift patches are prone to triggering. Wherever moistness reaches down to ground level on steep grass-covered slopes, small glide-snow avalanches cannot be ruled out.
On sunny slopes the ground is bare of snow up to high altitudes. The remains of the snowpack are melt-freeze encrusted in early morning. Due to solar radiation, bonding disperses in near-surface snow, it turns to firn snow and the snowpack becomes more and more moist/wet. On shady slopes there is dry powder atop a compact snowpack. Near ridgelines there are older, brittle snowdrift accumulations which are prone to triggering in places.
Avalanche danger remains low