Regions
Northwest Inland.
Forecast snowfall amounts are uncertain for Wednesday night and Thursday. If more than 10cm falls, the avalanche danger may be higher than posted.
Confidence
Moderate - Intensity of incoming weather systems is uncertain on Thursday
Weather Forecast
Generally light snowfall (5-10cm) is expected on Thursday. A dry ridge should develop on Friday bringing mainly clear skies while overcast conditions are forecast for Saturday. Ridgetop winds should be moderate from the southwest on Thursday and then become light for Friday and Saturday. Daytime freezing levels are forecast to hover between 1100 and 1200m for the forecast period.
Avalanche Summary
In recent days a natural cornice fall triggered a size 3 slab avalanche in the southwest corner of the region. The avalanche occurred on an east aspect in high alpine terrain and stepped down to a few persistent weak layers from January and December. This avalanche demonstrates how a cornice fall can trigger layers that may otherwise be difficult to trigger. New wind slab activity is expected in response to new snow and strong winds on Wednesday and Thursday morning.
Snowpack Summary
As of Wednesday morning, up to 5cm of new snow had fallen with moderate to strong southerly winds. At treeline and in the alpine small wind slabs are expected to have formed. These wind slabs overlie a variety of surfaces which include a hard crust on solar aspects above 1300, moist or refrozen snow on all aspects below 1300, and settled wind slabs in exposed high elevation terrain. A layer of surface hoar from early March can be found down 50-70cm 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 are generally dormant but could wake up with substantial warming or a heavy trigger (like a cornice fall). Basal facets exist in most areas and have recently been reactive in the north of the region
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.