Regions
Northwest Inland.
Lingering slabs and cornices will become weak with sun exposure. Extra caution is required on sun exposed slopes during the heat of the afternoon.
Confidence
Moderate - Timing or intensity of solar radiation is uncertain
Weather Forecast
A mix of sun and cloud is expected for Sunday with freezing levels around 1100m in the afternoon and moderate alpine winds from the south. A mix of sun and cloud is expected for Monday with the possibility of scattered flurries. Afternoon freezing levels are expected to be around 1000m and alpine winds are forecast to be light from the south. Light snowfall is currently forecast for Tuesday with freezing level around 1000m and moderate alpine wind from the southwest.
Avalanche Summary
On Friday, a two natural avalanches were reported from steep south facing terrain in the alpine north of Smithers. One was a size 1.5 and the other was a size 3. Skiers were triggering small size 1 slabs with a thickness of 10cm. In the for north, a natural size 2 cornice release was reported. On Thursday, a MIN report from Smithers (https://goo.gl/ssYcRw) describes a natural size 1.5 wind slab that released on a southeast aspect at 1600m and was 30cm thick. Natural activity was also heard but not observed from cliffy terrain in the south of the region. On Wednesday, a few natural wind slabs up to size 2.5 were observed in steep wind-loaded alpine terrain in the south of the region. There was also a large cornice fall that did not trigger a slab on the slope below. In the northern part of the region there were some reports of solar induced slabs to size 3 on south aspects, and natural cornice falls. One cornice fall triggered a size 4 avalanche that released on the ground and cleaned out an entire bowl. It was 1km wide and ran 1.5km.
Snowpack Summary
Roughly 20-40 cm of snow has fallen in the past week, with the highest accumulations occurring in the southwest of the region. Strong ridgetop winds have shifted the new snow into hard or soft wind slabs in exposed terrain, adding to an ongoing wind slab problem. A layer of surface hoar from early January can be found in isolated locations between 60 and 140 cm down. There hasn't been any activity reported on this layer for a couple of weeks now and it is becoming less of a concern. In shallower areas the snowpack sits on a weak base layer of facetted snow. Recently, this layer has been active in the north of the region, responsible for several large avalanches in unsupported alpine terrain.
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.