Boletín de aludes

Kootenay Boundary

Dec 26 – 27, 2014Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Sun
Mon
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
3 · Notable
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Lo esencial

Jump over to avalanche.ca/blogs to learn more about the persistent slab problem.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–4
    Watch for isolated wind slabs in exposed terrain at and above treeline. Reverse winds forecast for the next few days will likely form wind slabs in unusual locations.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    2–5
    A slab 30 - 70 cm in depth remains sensitive to human triggering. This problem isn't likely to go away any time soon.

Confidence

Fair - Due to the number of field observations

Weather Forecast

Synopsis: Light precipitation is possible Saturday afternoon as a weak system passes over the SE portion of the province. On Sunday a strengthening ridge of high pressure drives cold and dry conditions that will likely persist for the next week. Saturday: Freezing Level: Valley Bottom; Precipitation: 2-5mm | 2-10cm; Wind: Treeline: Light, SW | Ridgetop: Strong, W.Sunday: Freezing Level: Valley Bottom; Precipitation: Trace; Wind: Treeline: Light, E/NE | Ridgetop: Moderate to Strong E/SE.Monday: Freezing Level: Valley Bottom; Precipitation: Nil; Treeline: Moderate, NE | Ridgetop: Moderate, NE.

Avalanche Summary

On Thursday a party of skiers triggered a size 2 avalanche on a SW facing slope around 1800m in the Nelson area. Two people were reportedly caught and carried but thankfully ended up on the surface as everything came to a stop. This type of activity is likely to persist for the foreseeable future.

Snowpack Summary

30 - 70 cm of snow from the last week is consolidating into a slab above a touchy weak layer formed in mid-December consisting of surface hoar sitting on a thick rain crust. This combo is thought to extend as high as 2400 m. This layer will likely remain sensitive to human triggering for the foreseeable future. High elevation north facing slopes likely do not have the rain crust, but are still reported to have touchy buried surface hoar. On these slopes, deeper facets or buried surface hoar from earlier in the month may also be lurking. At the base of the snowpack, a crust/facet combo appears to have gone dormant for the time being.

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