Confidence
Fair - Timing or intensity of solar radiation is uncertain on Wednesday
Weather Forecast
Wednesday: increased cloud with light precipitation developing in the late afternoon becoming moderate in some areas overnight / moderate southerly winds / freezing level at 2800m Thursday: light precipitation / moderate westerly winds / freezing level at 1700m Friday: a mix of sun and cloud / moderate westerly winds / freezing level at 1700m
Avalanche Summary
Over the past few days, many small and large wet loose snow avalanches occurred in response to daytime warming and direct solar radiation. Numerous size 2-3.5 slab avalanches also occurred on sun-exposed aspects, with more isolated activity on shaded aspects. One report indicated a wet loose snow avalanche that triggered a slab that most likely ran on the mid-February surface hoar.
Snowpack Summary
Up to 80cm of snow overlies a weak layer of facetted crystals sitting on a crust in the alpine and at treeline. This layer still reacts to snowpack testing producing sudden, "pop" results. Recent reports of remotely triggered avalanches are noteworthy and suggest the problem will not heal quickly. Wind slabs are reported to be isolated to the immediate lee of exposed features at high elevations. Spring-like, moist snow exists on all south facing slopes as well as many north facing areas with limited crust recovery developing at night. There is still concern for the mid-February buried surface hoar layer that is down about 140-220 cm. Avalanches releasing on this layer are a low probability-high consequence situation. Cornices in the region are very large. With warmer temperatures, and longer periods of direct solar radiation, these may become weak and fail. They could provide a large enough trigger to release these deep layers on slopes below. Cornices are large and sagging due to recent warm temperatures.
Problems
Wet Slabs
Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
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.