Avalanche Forecast

Good - -1

Wednesday: Mostly dry. Light northerly winds. Alpine temperatures around -12C. Thursday: Dry. Winds becoming westerly. Remaining cold, but a mild inversion could locally elevate alpine temperatures by a few degrees. Friday: light snowfall with around 5 cm expected. Moderate NW winds. Alpine temperatures around -12C.

Both natural and human-triggered avalanches up to size 2.5 continue to be reported in the Monashees and Selkirks, releasing on the surface hoar layer from mid-December. Notable is the wide distribution, with avalanches reported on all aspects and elevations from 1400 to 2300 m. In the north of the region, fractures are typically 30-40 cm deep, although one was reported to have a fracture line up to 70 cm deep. In the south of the region, typical fracture depths are more like 20 cm. Several remote-triggered avalanches occurred, where the avalanche was triggered by someone riding some distance from where the slide occurred. Sympathetic avalanches were also reported, where one slide initiated other avalanches. With further snowfall, the current pattern of avalanche activity will continue, but the size and destructive force will go up.

A north-south split exists in this region at present as a result of the track of recent storms. Northern and western areas have seen up to 50 cm of recent storm snow, while areas further south have seen more like 20cm. This storm slab is reported to be upside-down, which means higher density snow sits on top of less dense snow. The storm slab sits above a well developed surface hoar layer from mid December, which has been reacting readily to snowpack tests and ski cutting. Additionally, remote-triggered avalanches have been reported on this layer, indicating it has a high potential for fracture propagation. All this info points to the same thing: Where the storm slab is sufficiently thick (in the order of 40 cm) and cohesive, conditions are ripe for slab avalanches. Lower in the snowpack, the mid-layers are well-consolidated and strong. Near the base of the snowpack there are a few layers that have the potential to wake up with a really big storm or very heavy loads (such as a sled airing off a cornice). These include a surface hoar layer from early November, a crust/facet combo from October and the interface on steep glaciated terrain with snow that did not melt over the summer.