Regions
Northwest Coastal.
The recent stormy weather has dumped as much as 100 cm of new snow on last week's crust. This has created storm slabs and there have been reports of large natural avalanches. The new snow will take some time to settle.
Confidence
Moderate - Due to the number of field observations
Weather Forecast
THURSDAY: Flurries, accumulation 5-10 cm, Moderate southwest wind. Alpine temperature -5. Freezing level 800 m.FRIDAY: Flurries, accumulation 10-15 cm, Moderate southwest wind. Alpine temperature -7. Freezing level 500 m.SATURDAY: Mix of sun and cloud. Light to moderate north west wind. Alpine temperature -7. Freezing level 300 m.
Avalanche Summary
Natural avalanche activity in the alpine to Size 2 was reported west of Kasiks on Tuesday morning. Also on Tuesday skiers in the Shames area reported "hearing a large avalanche" from a valley adjacent to the ski area. In recent days other observers in the Terrace area report shooting cracks within the recent storm snow (see the Mountain Information Network (MIN) post from Nov 25). Continued snow and wind are expected and the recent storm snow will take some time to settle. Travel in avalanche terrain will require very conservative route-finding and terrain choices. Please post your observations to the MIN.
Snowpack Summary
Recent stormy weather has brought about 90-130 cm of storm snow to the southern part of the region and now lies on the supportive 5-10 cm thick, November 23 rain crust from last week. Below this crust is a weak layer that formed in late October and is now buried 120-160 cm within the snowpack. Beneath this October crust is a 20-30 cm thick layer consisting of several thin crusts and facets. Recent snowpack tests report easy to moderate, sudden compression test results within the storm snow as well as moderate to hard, sudden results on the October 31 layer near the base of the snowpack.Across the southern part of the region snowpack depths average about 120 m at 800m elevation, and up to 180 cm at 1200 m. Reports from the north near Ningunsaw, describe a a much shallower snowpack. Here, a possible 30-40 cm of recent storm snow may now overlie a thin lower snowpack composed mainly of facetted snow. Snow depths in this part of the region range are from 60-120 cm between 600 and 1100 m elevation.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.
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.