Regions
Kootenay Boundary.
Keep your terrain selection in sync with the bonding of the recent storm snow. Remember that this bond is likely to vary with elevation and aspect.
Weather Forecast
Sunday night: Scattered flurries bringing approximately 5 cm of new snow. Light to moderate south winds.Monday: Mainly cloudy with isolated flurries and a trace of new snow. Light southwest winds. Freezing level to 1700 metres with alpine temperatures around -2Tuesday: Mainly cloudy with isolated flurries and a trace of new snow. Light to moderate southwest winds. Freezing level to 1600 metres with alpine temperatures around -3.Wednesday: Cloudy with flurries bringing approximately 10 cm of new snow. Moderate to strong southeast winds. Freezing level to 1600 metres with alpine temperatures around -2.
Avalanche Summary
Reports from Saturday showed storm slabs releasing from Size 1-2 with ski cutting and explosives control. One natural Size 1.5 slab was observed on a steep northeast slope. Crown fractures generally ranged from 10-40 cm. Natural loose wet avalanches were noted reaching to Size 1.5 in the Kootenay Pass area.
Snowpack Summary
Stormy weather over the past week brought roughly 40-50 cm of snow to the region. Periodic high freezing levels and solar exposure over the same period formed a series of crusts (March 19-24) that exist within this upper snowpack at lower elevations and on solar aspects. The new snow and series of crusts lie over a more widespread (March 14) rain crust that exists at all elevations. Moist or wet snow exists below this rain crust. The late-February facet / surface hoar interface (90-140 cm deep), the mid-February crust (110-150 cm deep), and basal facets in shallow snowpack areas may still be present at upper elevations. Overlying crusts have been noted acting as a bridge over these layers and any remaining reactivity is likely limited to high alpine locations.
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.