Avalanche danger above 2000m is moderate, below that altitude danger is low. Snowdrift accumulations are problematic. Small slab avalanches can be triggered even by one sole skier. Danger zones occur in steep ridgeline terrain on W/N/E facing slopes and in wind-loaded gullies and bowls. Give consideration to the risks of being swept alone and forced to take a fall.
Snowpack
In northern aspects snowdrifts have been deposited atop an irregular snowpack and can be prone to triggering, particularly if the old snowpack in shady regions is expansively metamorphosed. At high altitudes, in addition, trigger-sensitive intermediate layers in the uppermost part of the snowpack have persisted. Larger fractures over wide surfaces are unlikely. On south-facing slopes there is little snow on the ground, usually encrusted in the early morning hours, then softening later on. In wind-exposed terrain, the snowpack surface is wind-pressed; on shady slopes there is still loosely-packed zone atop a stable old snowpack fundament in wind-protected zones.
Tendency
Avalanche danger levels are expected to recede again.
Danger level
2000m
Avalanche Problem
Persistent weak layer
2000m
Caution urged towards the risks of taking a fall
Avalanche danger is low. Locally, weak layers in the old snowpack can be problematic. Small slab avalanches can be triggered in isolated cases by large additional loading, which happens more likely in places with little snow. Avalanche prone locations occur in extremely steep ridgeline terrain in W/N/E aspects as well as at entries into gullies and bowls. Dangers of being swept away and of taking a fall outweigh those of being buried in snow masses.
Snowpack
The snowpack is stable by and large. At high altitudes, foehn winds have generated shallow snowdrifts on north-facing slopes. In addition, trigger-sensitive intermediate layers in the uppermost part of the snowpack have persisted. Fracture propagation is unlikely. On south-facing slopes there is little snow on the ground, mostly encrusted in the morning hours before softening up later on. In wind-exposed terrain the surface is wind-pressed, on shady slopes with little wind there is still loosely-packed snow.