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Avalanche Forecast

Archived

Mar 5th, 2017–Mar 6th, 2017

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Kootenay Boundary.

Large storm slabs were reactive over the weekend and there's some uncertainty about how long they will persist. Cautious decision making and conservative terrain selection is recommended.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

An unsettled pattern opens the door to a string of relatively small low-pressure systems that should deliver modest snowfall to the region through the forecast period. MONDAY: Scattered flurries with 2-8 cm of new snow, moderate southwest winds, alpine temperatures around -10 C.TUESDAY: Scattered flurries with 2-6 cm of new snow, moderate southwest winds, alpine temperatures around -10 C.WEDNESDAY: 5-15 cm of new snow, moderate southwest winds, alpine temperatures around -10 C.

Avalanche Summary

A widespread natural avalanche cycle occurred on Friday night into Saturday morning, with size 2-3 storm slab avalanches on a variety of aspects and elevations. Some crowns were over a metre thick, but observers suspect the slabs failed within the storm snow and did not step down to any deeper layers. Storm slabs were also reactive to human triggers, producing size 1-1.5 slab avalanches on convex and wind-loaded features at treeline (30-60 cm deep). Natural activity has likely tapered off, but storm slabs will likely remain primed for human triggering.

Snowpack Summary

A wide-ranging 35 to 100 cm of snow has fallen in the past week. The new snow is rapidly settling into a denser slab which sits over a variety of old interfaces including sun crusts, surface hoar, and weak faceted snow. Winds shifted from the northwest to the southwest during the storm, forming thicker deposits in lee areas at higher elevations. The new snow also has the potential to wake up the mid-February crust layer buried about a metre deep on solar aspects and at lower elevations. Areas with a shallow snowpack (less than around 170 cm) generally have a deep persistent weakness of facets near the ground. There are a number of great MIN reports from Thursday and Friday here.

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.