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Avalanche Forecast

Jan 3rd, 2012–Jan 4th, 2012
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
4: High
The avalanche danger rating at treeline will be high
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable
Alpine
4: High
The avalanche danger rating in the alpine will be high
Treeline
4: High
The avalanche danger rating at treeline will be high
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: Sea To Sky.

Confidence

Good - -1

Weather Forecast

Wednesday: Continued very heavy precipitation with up to 60-80cm of new snow expected for immediate coastal areas, but less as you move inland. Freezing levels as high 1700m but dropping throughout the day, and strong to extreme southwesterly winds. Thursday: another 10-20cm possible but tapering off throughout the day. Freezing levels as high as 1000m and moderate to strong southwesterly winds. Friday: Relatively dry, cold and calm.

Avalanche Summary

Persistent slabs and wind slabs are primed for human-triggering and heavy loading from snow wind and rain will likely cause natural avalanches. Three separate serious incidents that are relevant for the Sea-to-Sky region occurred on Monday afternoon in the Duffey Lake and Southern Chilcotin areas of the South Coast Inland region. All of incident sites had similar terrain characteristics with north through east facing steep treeline features. Two of the avalanches likely involved the mid-December persistent weakness, while the third was reported to have released on basal facets in a shallow snowpack area with a 50-75cm depth. All of the avalanches resulted in serious injury and at least two of them were human-triggered.

Snowpack Summary

The snowpack structure is highly variable and complex. Gusty winds are keeping wind slabs and cornices fresh and weak. Slabs overlaying various old snow surfaces, including crusts, facets, and surface hoar, buried mid-December are primed for avalanches in many parts of the region. The surface hoar is lurking generally down 80-100cm in sheltered treeline areas and below. In exposed treeline and alpine areas, weak facets with associated crusts are down generally 80-120cm, but wind-loading has resulted in highly variable slab thicknesses. A recently buried thin hard rain crust that extends into alpine elevations is also providing a poor bond to the overlying slab. Basal facets remain a concern in shallow snowpack areas, especially where the snowpack is overlaying summer firn on slopes that have already produced deep persistent slab avalanches and have been reloaded.

Avalanche Problems

Wind Slabs

Fresh wind slabs are lurking below ridgecrests, behind terrain features and in cross loaded gullies.

Aspects: North, North East, East.

Elevations: Alpine, Treeline.

Likelihood: Likely - Very Likely

Expected Size: 2 - 5

Storm Slabs

Weaknesses within and under recent and new storm snow are susceptible to natural and human triggers.

Aspects: All aspects.

Elevations: All elevations.

Likelihood: Likely

Expected Size: 2 - 5

Persistent Slabs

Persistent weaknesses will probably play a roll in avalanche activity over the next couple of days. Very large avalanches running to valley bottoms are likely.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood: Likely

Expected Size: 3 - 7