Boletín de aludes

Kootenay Boundary

Mar 24 – 25, 2012Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Mon
Tue
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
3 · Notable
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Lo esencial

This is the first big warm-up after some significant snowfall. A warming-related avalanche cycle is expected.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–6
    Cornices are very large and may fail with daytime warming. There is potential for triggering deep slabs on underlying slopes.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    Warm temperatures and solar radiation are triggering wet sluffs. These small avalanches may trigger the deeper weaknesses.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    3–8
    The deep nature of the mid-February surface hoar layer makes potential avalanches triggered on this layer large and destructive. Avoid thin snowpack areas where triggering is more likely.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Sunday: Expect clouds to build through the day, with freezing levels reaching 2500m under light southerly winds. Monday & Tuesday: Continued clouds with light flurries possible. Winds remain light southerly and freezing levels may reach 1500m.

Avalanche Summary

We have reports of loose, moist avalanches being triggered by solar radiation on sunny slopes. A fatal avalanche incident occurred in this region on Wednesday. We will post more details when they become available.

Snowpack Summary

The warm temperatures have brought us into a spring melt freeze cycle with the surface snow softening with daytime warming on solar aspects then crusting overnight as temperatures dip back below freezing. On north aspects, the surface snow remains cold. Up to 60 of recent storm snow is settling quickly with the warm temperatures and this most recent storm interface is gaining strength. The early February surface hoar lingers, down 100-180cm. Although the avalanche activity has become more sporadic on this layer, triggering it would yield a very large destructive avalanche.

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