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Avalanche Forecast

Dec 5th, 2013–Dec 6th, 2013
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
1: Low
The avalanche danger rating below treeline will be low

Regions: South Columbia.

Confidence

Fair - Due to the number of field observations

Weather Forecast

A strong Arctic air mass will continue to dominate conditions in the southern interior. Friday: Mostly sunny, light NE alpine winds, alpine temperatures -20 to -25CSaturday: Mostly sunny, light-moderate NE alpine winds, alpine temperatures as low as -30CSunday: Increased cloud cover, moderate alpine winds, alpine temperatures as low as -25C, very light snowfall possible

Avalanche Summary

Fewer natural avalanches are occurring in the region but a few natural slab avalanches up to size 2 have been reported. These are both wind slabs and previous storm snow sliding on the late-November crust/surface hoar interface.

Snowpack Summary

Snowpack depths are typically 100-140 cm at treeline elevation. The previous storm snow (~30-60cm) overlies the late-November interface which typically consists of sun crusts on steep south facing slopes and surface hoar in sheltered areas. These weak layers are expected to be persistent and will continue to create avalanche problems in areas with enough overlying snow. The current cold temperatures will contribute to the persistence of this weak layer. Strong NE winds after the storm have caused reverse loading and wind slab formation on SE through W aspects in wind exposed areas. There are two layers of concern within the mid/lower snowpack but these have recently become inactive: the early November surface hoar is roughly 60cm above the ground and the October rain crust is at the base of the snowpack. While these layers have recently become inactive, residual risk of large, destructive avalanches exists, especially in areas with a thinner snowpack. The October crust can be found in the alpine on north aspects and the early November surface hoar appears to be isolated and drainage specific.

Avalanche Problems

Wind Slabs

Strong NE winds have redistributed loose surface snow into reactive wind slabs on southwest facing terrain. This is an atypical loading pattern which has the potential to catch skiers/riders by surprise.
Be cautious as you transition into wind affected terrain.>Avoid travelling in areas that have been reverse loaded by winds.>

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

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 1 - 3

Persistent Slabs

This persistent slab will be tricky to manage as it overlies a variety of weak surfaces. A conservative and investigative approach is required for safe mountain travel.
Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.>Dig down to find and test weak layers before committing to a line.>

Aspects: All aspects.

Elevations: All elevations.

Likelihood: Unlikely - Possible

Expected Size: 2 - 4