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Avalanche Forecast

Archived

Mar 4th, 2022–Mar 5th, 2022

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

Regions

Little Yoho.

The persistent layer continues to be a concern, few avalanches have been reported from this interface but the potential consequences are high. LB

Weather Forecast

Relatively benign weather over the next few days, we will see temperatures varying from -15 to -5 with light to moderate winds. Some sporadic snowfall with small amounts expected.

Snowpack Summary

5-10 cm of new snow overlies a melt freeze crust from Thursdays warming, this crust can be found up to 1900m on solar aspects. Above 1900m, 40-60 cm of previous storm snow has solidified into a slab overlying a suncrust buried on February 16. This combination should now be watched closely, as it produces whumphs and tests indicate propagation.

Avalanche Summary

No new avalanches observed or reported today, but whumphs (unstable snow) observed on Hawk Ridge in Kootenay Park on Thursday. On Wednesday in Kananaskis Country, a size 2.5 skier remote slab 40 cm deep was triggered on a SE aspect at 2500 m (ran on the Feb. 16 crust).

Confidence

Due to the number of field observations

Problems

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.