Regions
Northwest Inland.
Lingering wind slabs and cornices are expected to become weak with sun exposure and afternoon warming. Use extra caution on sun exposed slopes when the solar radiation is strong.
Confidence
Moderate - Timing or intensity of solar radiation is uncertain
Weather Forecast
A mix of sun and cloud is expected for Wednesday with afternoon freezing levels around 900m and light alpine winds from the northwest. Sunny conditions are expected for Thursday with afternoon freezing levels around 1100m and light outflow winds in the alpine. A mix of sun and cloud is forecast for Friday with freezing levels climbing to around 1500m and moderate outflow winds in the alpine.
Avalanche Summary
On Monday, a natural cornice release triggered a size 1.5 wind slab on a northwest aspect at 1750m which was 25cm thick. Skiers were triggering size 1 soft slabs on steep leeward slopes. In the far north of the region, a natural cornice release triggered a size 2.5 slab which released on the early March surface hoar layer.
Snowpack Summary
In sheltered areas at higher elevations, 20-30cm of low density snow can be found. Recent southerly winds have redistributed the surface snow in exposed terrain formed wind slabs and cornices in leeward terrain. On Monday, moist snow was reported up to 1650m elevation on southern aspects and up to 1200m on northern aspects. A layer of surface hoar from early March can be found down 60-80cm but only seems to be a problem for the northern half of the region. Professional operators are still tracking two deep weak layers from early-January and early-February which can be found down about 1m or more. These layers have been dormant for a couple weeks but could wake up with heavy storm loading, substantial warming, or a heavy trigger like a cornice fall. In the far north of the region, there is an isolated weakness at the base of the snowpack that has been responsible for some very large and destructive avalanches.
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.