Boletín de aludes

Kootenay Boundary

Dec 12 – 13, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

Sat
Sun
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil
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Lo esencial

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Light amounts of new snow and wind may have created thin new windslabs at high alpine elevations adding to an existing windslab problem. Watch for triggering in gullies and behind ridge crests.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–4
    A weak interface buried at the end of November is now buried by up to 60cm of snow. Triggering this layer may be more likely in steep, unsupported terrain, and in areas where the overlying snow has settled into a cohesive slab

Confidence

Fair - Due to the number of field observations

Weather Forecast

Friday: Trace amounts of new snow / Light west winds / Freezing level at 1100mSaturday: Light snowfall / Strong west winds / Freezing level at 1100mSunday: Light snowfall / Moderate southwest winds / Freezing level at 1500m

Avalanche Summary

Small wind slab avalanches have been observed at treeline and in the alpine around Nelson and in the Kootenay Pass area.

Snowpack Summary

Dribs and drabs of recent snowfall now overlie generally faceted surfaces that formed during the recent cold snap. At the same buried interface you may find small surface hoar on sheltered slopes or windslabs in exposed alpine terrain. In some high elevation terrain the new snow may have been shifted into pockets of small windslabs.Between 50 and 70cm below the surface you may find a weak layer of surface hoar on sheltered north facing slopes and a crust on steep solar aspects. In some areas the overlying snowpack has not yet settled into a cohesive slab required for slab avalanche activity. There are reports of a deeply buried early season crust that formed in October, this layer is more likely to be found in the high alpine on northerly aspects. Little is known about its reactivity in this region.

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