Avalanche danger is low. In ridgeline terrain, in gullies and bowls, freshly generated snowdrift accumulations require caution. They are mostly small-sized, but poorly bonded with the old snowpack and thus, prone to triggering. In risky terrain for falls, evaluate the drifts with caution, small-sized - avalanches can be triggered by one sole skier. Glide-snow avalanches still possible.
Snowpack
The uppermost snowpack layers are generally still loose (except in wind-impacted terrain) and lie atop a well consolidated and often encrusted old snowpack . In high-altitude wind-impacted zones and ridgelines, small fresh snowdrift accumulations have been generated. Some older drifts are now blanketed and layers of graupel embedded. Not much snow on the ground at low altitudes.
Tendency
Avalanche danger levels will continue to be favorable
Danger level
2200m
Avalanche Problem
Wind slab
2200m
Generally favorable conditions, low-to-moderate avalanche danger
Small-area fresh and older trigger-sensitive snowdrift accumulations are the main danger. Danger zones occur in wind-loaded steep terrain, in gullies and bowls, and behind protruberances in the landscape. Size and frequency of danger zones tend to increase with ascending altitude. In addition, on steep shady slopes at high altitudes and in transitions from shallow to deep snow, isolated slab avalanches can be triggered by large additional loading. A cautious route selection is advised. Small-to-mediium glide-snow avalanches are possible only in isolated cases. Caution urged below glide cracks.
Snowpack
The uppermost snowpack layers are generally still loose (except in wind-impacted terrain). In high-altitude wind-impacted zones and ridgelines, small fresh snowdrift accumulations have been generated. Some older drifts are now blanketed and layers of graupel embedded. More deeply embedded layers inside the snowpack are unlikely to trigger, at most where the snow is shallow and on very steep shady slopes.
Tendency
At high altitudes, caution urged towards small snowdrift accumulations.
