Avalanche Forecast

Low - Due to the number of field observations

WEDNESDAY NIGHT: Cloudy with flurries, trace to 10 cm accumulation. Moderate southwest wind. Freezing level below 600 m.THURSDAY: Periods of snow, 5-15 cm accumulation. Light to moderate south-southwest wind. Freezing level 600 m.FRIDAY: Snow, 15-35 cm accumulation. Moderate south-southwest wind with strong to extreme gusts. Freezing level rising above 1000 m.SATURDAY: Periods of snow, 10-45 cm accumulation. Moderate gusting strong west-southwest wind. Freezing level dropping below 1000m.

On Sunday, explosives were able to trigger wind slab avalanches to size 1.5. Additionally, a large (size 2) natural wind slab avalanche was observed on a northeast aspect. On Monday, wind-loaded pockets were reactive to skier traffic, including 2 very small unsupported pockets remotely triggered (from a distance) by skiers.Information from this region is limited. Tell us what you see by posting to the Mountain Information Network MIN.

Up to 20 cm of new snow sits on a melt-freeze crust at elevations below approximately 1000 m. Above 1000 m, this new snow is just adding to the 150+ cm of recent snowfall from over a week ago. Moderate to strong winds have redistributed recent snow and formed wind slabs at upper elevations, especially in lee and cross-loaded features. Expect to find more reactive slabs in wind loaded areas, and especially in places that receive higher snowfall amounts.A total 120-200 cm of mid-December snow sits on a weak layer of surface hoar (feathery crystals), facets (sugary snow), and crusts. This layer was initially a concern when snowfall first accumulated, but the strength of this layer has generally improved. The surface hoar is most prevalent and has most recently been reactive between 1100-1300 m in more northern portions of the region, and is something to keep in mind if you plan to travel to areas like Ningunsaw.Deeper in the snowpack, there are several crusts, including an early season crust with facets near the bottom of the snowpack.