Confidence
Fair - Due to variable weather conditions
Weather Forecast
A series of Pacific frontal waves and upper troughs will bring continued unsettled weather through the forecast period. Light -moderate precipitation amounts can be expected daily. With fast moving systems, timing seems to be hard to pinpoint. A strong upper SW flow will provide warmer the normal temperatures, rising freezing levels in the afternoon, then falling during the night. Things should start to cool off significantly by Friday. Wednesday: Snow amounts 5-15 cm above 1200 m. Ridgetop winds moderate from the SW. Freezing levels 1500 m. Thursday: Snow amounts 8-15 cm. Ridgetop winds strong from the SW. Freezing levels 1600-1800 m. Friday: Light bands of precipitation, and cloud cover.
Avalanche Summary
On Monday several large natural solar induced cornice releases were reported. These occurred on NW-NE slopes from 2000 m- 2400 m. To note, none of theses cornice falls stepped down to the deeply buried persistent weak layer. I still wouldn't rule out the potential, as we saw that layer reactive only 4 days ago. Numerous loose wet avalanches were also reported on Monday on various aspects, running up to size 2. This could continue in your local mountains if the sun is able to poke through the clouds over the next few days. On Saturday three, size 3 natural avalanches were observed in steep, rocky, unsupported terrain. They occurred between 2000-2800m on north to east aspects and are suspected to have run on the February persistent weak layer.
Snowpack Summary
Recently formed variable wind slabs exist in the alpine and at treeline. Over the past several days, spring-like conditions have influenced the snowpack. Solar radiation has led to moist surfaces on sun exposed slopes up to ridgetop, other aspects moist below 1500 m. Crust recovery developing at night. Cornices have grown large and have become unstable; they may act as a large trigger on slopes below. A consolidated slab overlies a persistent weak layer that was buried in early February. Now 1-2 m below the surface, these weaknesses include surface hoar, facets or crusts. Concern still exists potentially for deep and destructive releases at this interface. This may be a low probability, high consequence problem that may require a large trigger.
Problems
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.
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.