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Avalanche Forecast

Archived

Mar 29th, 2014–Mar 30th, 2014

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

Regions

Kootenay Boundary.

Confidence

Fair - Forecast snowfall amounts are uncertain on Sunday

Weather Forecast

Sunday: Cloudy with light snowfall possible. Light southerly winds. Freezing level 1400m.Monday: Mix of sun and cloud. Light west winds. Freezing level 1500m.Tuesday: Mainly sunny with some cloudy periods. Light westerly winds. Freezing level 1800m.

Avalanche Summary

Recent avalanche activity has been reported as loose dry and moist avalanches running to size 1.5 in steep terrain.

Snowpack Summary

Up to 25cm of recent new snow sits on top of a melt-freeze crust formed on March 25 on all aspects except steep north at tree-line and above. There is now 60 - 90cm of new snow on top of the March 10th crust. This crust is widespread to 2000m across the region, perhaps even higher on solar aspects. There are reports of the crust being as thick as 15cm in the south of the region, however there seems to be variability in how thick and supportive it is. As you head north in the region where the mountains are higher (temperatures were colder when the crust was forming) this crust is less likely to exist. If you are heading to the north of the region make sure you check out the South Columbia bulletin also.A facet/crust persistent weakness buried at the beginning of February, now down 70 - 200cm, has been highly variable in terms of reactivity but still shows 'sudden' results in some snowpack tests. In areas where the strong and supportive crust exists, triggering this layer has become unlikely. That said, any avalanches triggered on this deep persistent layer would be large and destructive.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.