Warm temperatures and solar input will drive the hazard this weekend. Pay close attention to sun affected slopes
Confidence
Moderate - Timing or intensity of solar radiation is uncertain
Weather Forecast
A modified, dry arctic air mass remains over the much of the province. Expect valley fog in the morning at lower elevations and sunshine in the alpine for most of the interior of BC. Moderate temperatures aloft, with above freezing layers of warm air, will pass through the Province during the weekend. For more in-depth weather information visit: https://avalanche.ca/weather
Avalanche Summary
Several small loose dry avalanches, small soft slab avalanches, and 1 large glide-crack release have been reported over the last couple of days. Continued warming in the alpine combined with sunny conditions could result in loose natural avalanches from steep south-facing slopes. Recent storm snow will begin to show slab properties as it settles with the warm temperatures.
Snowpack Summary
20-40 cm of settling low density snow overlies a generally strong snowpack. You may encounter wind slabs which are sensitive to the weight of a person near ridge tops. Recent storm snow may sluff in steep terrain, especially with a touch of sun. The lower snowpack is reportedly well settled. The early December weak layer (about 80-150 cm down) is spotty in distribution, but where it does exist still gives hard, sudden results, meaning it is unlikely to be triggered, but could produce a very large avalanche.
Problems
Loose Dry
Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.
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.