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Avalanche Forecast

Feb 27th, 2012–Feb 28th, 2012
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate

Regions: South Columbia.

In your local area: Be wary of any slopes which are being warmed by direct sun, as this may weaken existing slabs and could cause natural avalanches.

Confidence

Good

Weather Forecast

Tuesday: Mainly sunny with valley cloud. Light southerly winds. Freezing level around 600m. Wednesday/Thursday: Cloud and flurries. Light south-west winds. Temperatures remain cool, except during sunny breaks, when some local solar warming may occur.

Avalanche Summary

Many large natural and human-triggered avalanches have been reported each day since Wednesday. Natural activity (up to size 3.5) spiked following the heaviest snowfalls on Tuesday night and Friday night. Skiers have been triggering avalanches (mostly size 1-2.5) accidentally and remotely. These are running on storm snow instabilities or persistent weaknesses in the upper snowpack. There have been some lucky escapes. Conditions will remain ripe for human-triggering after the more obvious signs of instability (like new snowfall, wind-loading and natural activity) die down.

Snowpack Summary

Recent storm snow totals of about 60-140cm sit above the Feb 16. surface hoar layer and the early Feb interface. The early Feb interface is a combination of weak layers: In most locations it marks a widespread surface hoar layer. On steep south- and west -facing aspects, a sun crust was also buried at the same time, meaning that most terrain in the region has a weak layer in the upper snowpack. Deep wind slabs exist on many aspects and cornices are large. Upper snowpack persistent weak layers are still very touchy, as evidenced by scores of remote and human-triggered avalanches over the past several days. Cornice fall and solar warming are my top current picks for further natural triggering of these weak layers, while human/machine-triggering remains likely on a variety of slopes.

Avalanche Problems

Persistent Slabs

Several weaknesses exist in the upper metre or so of the snowpack. These layers remain sensitive to triggers. Large, destructive avalanches could be triggered by the weight of a person, even from a distance.

Aspects: All aspects.

Elevations: All elevations.

Likelihood: Likely - Very Likely

Expected Size: 2 - 6

Wind Slabs

Wind slabs have grown large on many slopes. Persistent weak layers are buried beneath these slabs, meaning they could be touchy and create very large avalanches. Large cornices also threaten many slopes.

Aspects: North, North East, East, South East, South, South West, West.

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 1 - 5