Avalanche danger is low. Wet snow can be problematic. On extremely steep sunny slopes, isolated small wet loose-snow avalanches can trigger naturally. At intermediate altitudes esp. on E/W facing slopes, at high altitudes on south-facing slopes, where the moisture reaches ground level, small glide-snow avalanches cannot be ruled out on steep grass-covered slopes.
Snowpack
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, isolated snowdrift patches can be prone to triggering. Elsewhere there is dry powder atop a compact snowpack. On shady slopes where snow is shallow, isolated layers of faceted crystals have persisted inside the snowpack. Tests confirm that the snowpack is stable.
Tendency
Avalanche danger not expected to change significantly. As clouds move in, snow will moisten thoroughly also on shady slopes at intermediate altitudes (due to some rainfall).
Danger level
2000m
Avalanche Problem
Wind slab
2000m
Wet snow
Caution: small snowdrift accumulations at high altitudes
Avalanche danger is low. At high altitudes, small-area snowdrift accumlations can be prone to triggering as slab avalanches even by one sole person, esp. on very steep ridgeline terrain on NW/N/E facing slopes. Apart from the danger of being buried in snow masses, the risks of being swept along and forced to take a fall require adequate caution. On extremely steep sunny slopes, in addition, isolated small wet loose-snow avalanches can release during the course of the day. On steep grass-covered slopes, small glide-snow avalanches cannot be ruled out.
Snowpack
At high altitudes, shallow snowdrifts have accumulated, lie deposited atop faceted, expansively metamorphosed surfaces and are poorly bonded with them. On shady slopes where snow is shallow, isolated layers of faceted crystals persist more deeply embedded inside the snowpack, but they are unlikely to trigger. 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 becomes soft.
Tendency
Avalanche danger not expected to change significantly. As clouds move in, snow will moisten thoroughly also on shady slopes at intermediate altitudes (due to some rainfall).
