Avalanche Forecast
North Columbia
Although the temperature is forecast to remain cool at upper elevations, when the sun does come out it can have an immediate impact on those slopes directly facing it.
Avalanche Problem 1: Wind Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
Travel and Terrain Advice
- Extra caution needed around cornices with current conditions.
- Be cautious as you transition into wind affected terrain.
- Use ridges or ribs to avoid pockets of wind loaded snow.
Avalanche Problem 2: Persistent Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
A weak layer buried up to 80cm deep "woke-up" last week. This problem seems most reactive in south-facing terrain where buried crusts exist.
Travel and Terrain Advice
- Make observations and assess conditions continually as you travel.
- Watch convoluted terrain with variable snowpack depth and multiple trigger points.
- Pay attention to overhead hazards like cornices which could potentially trigger persistent slabs.
Avalanche Summary
Reports of avalanche activity on Friday and Saturday includes natural storm and wind slab avalanches to size 2 on north, south and west aspects from tree line into the alpine. On Friday there were two skier triggered size 2.5 persistent slab avalanche between 1800 and 1900m on south and southeast aspects. These ran on a crust buried mid-February 70cm deep and were in the northern part of the Monashee range.
Snowpack Summary
40 to 60 cm of storm snow from the past week has been redistributed into wind slabs in wind-exposed terrain on most aspects. Below this is a layer buried mid-February that presents as a sun crust on solar aspects, and spotty surface hoar on sheltered slopes. This layer looks most concerning on on solar aspects where it's associated with with small facets or surface hoar sitting above.
There are several deeper layers in the mid-pack that have shown signs of improving but remain on the radar as having a low probability of triggering yet would produce a high consequence avalanche if they are triggered. We're talking about surface hoar layer buried back in December and January. Near the base of the snowpack is a November crust combined with loose sugary snow. These layers may "wake-up" with strong inputs such as sustained warming, sustained snowfall, large triggers (e.g. cornice fall, smaller avalanches coming down from above); human triggering is also possible in shallow snowpack areas with variable snow depth and convoluted terrain.
Weather Forecast
MONDAY: Mix of sun, cloud and isolated flurries / Light to moderate west wind / Alpine temperature -12
TUESDAY: Mix of sun, cloud and isolated flurries / Light west wind / Alpine temperature -13
WEDNESDAY: Mix of sun, cloud and isolated flurries / Light southwest wind / Alpine temperature -8
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Shifting wind means there may be old buried wind slabs in places you don't expect them (as in reverse loading).