In the south of the region the main concern is fresh storm slabs as well as loose dry sluffing in the new snow.
In the north, the main concern is wind slabs at upper elevations only, so avalanche danger below treeline can be treated as LOW.
See the problems tab for more details.
A wind slab problem exists in the north of the region. Wind slabs may remain reactive especially where they sit over a crust on solar aspects, at ridgetops and roll-overs.
A storm slab problem exists in the south of the region, where recent snowfall has been significant (40-70 cm). Cooling temperatures will help to lock up storm slabs but some residual reactivity may still be observed in wind loaded features. Loose dry sluffing may also be observed in the new snow from overnight.
Sunday night: Mostly cloudy with flurries, up to 10 cm in the south, light northwest ridgetop wind, alpine temperature -15.
Monday: Mix of sun and cloud, light to moderate northwest ridgetop wind, alpine high -15.
Tuesday: Mix of sun and cloud, light northerly ridgetop wind, alpine high -22.
Wednesday: Sunny, light to moderate northerly ridgetop wind, alpine high -22.
Size 1 skier triggered wind/storm slabs have been reported every day since Thursday throughout the region. Check out this MIN report describing a skier accidental storm slab avalanche in the Coquihalla area Saturday.
Last week there were reports of natural, explosive and human triggered avalanches size 1-2, including a widespread natural avalanche cycle Monday night. Many of these failed on the recently buried persistent weak layer.
Snowfall in the south of the region is forecast to conclude Monday morning, after dropping 40-70 cm of snow over the last 72 hours. In the north, localized areas of soft wind slab may sit over a crust on solar aspects. Recent variable wind directions have resulted in wind loading in atypical terrain features.
30-80 cm of recent snow sits on a persistent weak layer that consists of facets at upper elevations, surface hoar in sheltered areas, a melt-freeze crust below 1600 m, and a sun crust on south-facing slopes.
In the south, the underlying snowpack is well consolidated. In the north, a melt-freeze crust from early December may be found 100 to 200 cm deep. Recent reports suggest that this layer is gaining strength and it has been unreactive in recent weeks.
