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Avalanche Forecast

Archived

Mar 3rd, 2019–Mar 4th, 2019

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.
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.

Wind slabs continue to be reactive at upper elevations. A persistent slab problem still exists in the region and has been responsible for sporadic human triggered avalanches over the past week.

Confidence

High - The weather pattern is stable

Weather Forecast

MONDAY: Mainly sunny / light to moderate east wind / alpine temperature -12 CTUESDAY: A mix of sun and cloud / light to moderate southeast wind / alpine temperature -8 CWEDNESDAY: Mainly cloudy with scattered flurries / light to moderate southeast wind / alpine temperature -6 C

Avalanche Summary

There is an excellent MIN post describing a skier triggered size 1.5 persistent slab avalanche on Saturday. Click here to see it. Additionally on Saturday reports indicate a few size 1-1.5 wind slab avalanches on west aspects in the alpine and treeline. There were reports of several size 1-1.5 explosives triggered storm slab avalanches on Friday in the alpine and tree line on northerly aspects.

Snowpack Summary

The surface consists of 15-30 cm of low density recent new snow. This new snow is sitting on old wind slabs and faceted (sugary) snow. A layer of feathery surface hoar sitting on a crust that was buried on February 7th is now 30-50 cm deep. Two other surface hoar layers are buried 50 to 80 cm down (referred to as the February 1st and mid-January layers) remain reactive in snowpack tests.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.