Boletín de aludes

Kootenay Boundary

Jan 11 – 12, 2015Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Tue
Wed
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
2 · Moderado
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Lo esencial

Check out this great video blog post which describes conditions in the Nelson area: http://backcountryskiingcanada.com/forums/view/safety-talk/avalanche-conditions-report-video-1

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    Storm accumulations from last week have likely gained considerable strength. That said, lingering wind slabs may still exist in the lee of ridge crests and terrain breaks.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–4
    Continued skier-triggered avalanche activity is a clear indication that weak layers, buried up to 120cm below the surface, have not gone away. I'd remain conservative in my terrain selection, and exercise cautious group management.

Confidence

Good

Weather Forecast

A dry ridge of high pressure will dominate the region for the period. Valley cloud should develop for most days, although generally clear skies are expected at higher elevations. Winds are forecast to remain light from the northwest, while freezing levels should hover at (or near) valley bottom.

Avalanche Summary

On Saturday, skiers triggered numerous persistent slab avalanches to size 2 in the north of the region, in some cases remotely from a distance of 10m. With the stable weather pattern, recent storm instabilities should become much less reactive; however, I would expect ongoing skier-triggered avalanche activity on the December persistent weak layers.

Snowpack Summary

A dusting of low-density snow overlies well-developed surface hoar which sits above a melt-freeze crust. The crust is reported to exist on all aspects below about 1900m, and on steep solar aspects at higher elevations. Stubborn wind slabs are likely in exposed alpine and treeline terrain. The main snowpack concern is a buried surface hoar layer (down 60-120 cm), which is sitting on a hard rain crust in some places. This widespread persistent weakness, which formed in December, exists at all elevation bands and remains a concern for triggering.

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