Watch for overhead cornices and use caution in wind affected alpine terrain.
Weather Forecast
SATURDAY: Mainly cloudy with a chance of flurries or showers. The freezing level climbs to 2100-2300 m and winds are light to moderate from the SE-SW. SUNDAY: Periods of light snow or rain – 5-10 cm/mm. The freezing level is near 1800-2100 m. Ridge winds are light to moderate from the S-SE. MONDAY: Cloudy with flurries. The freezing level is around 1600-1800 m and winds are light to moderate from the SW.
Avalanche Summary
Many areas reported widespread wind affected snow in alpine areas on Thursday. One reporter from the northern part of the region reported skier triggered soft slabs up to 30 cm deep (size 1-1.5). Cornices continue to pop off with regularity. Some are triggering slabs below and others are not. Some minor loose wet sluffing was also observed on sun-exposed slopes on Thursday afternoon.
Snowpack Summary
The snow surface consists of a sun crust or moist snow on sun-exposed slopes (depending on the time of day), dry settled powder on shady slopes (cool temperatures have maintained good snow quality), and pockets of fresh wind slab in lee and cross-loaded terrain features near ridge crests. In general, the snowpack is strong and well-settled throughout with no notable persistent weaknesses. Cornices are reported to be large and fragile.
Problems
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.