Boletín de aludes

Kananaskis

Feb 5 – 6, 2018Alberta Parks
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Archivado · caducó 9 years ago

Peligro de aludes

Wed
Thu
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
3 · Notable
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Lo esencial

Avoid avalanche terrain. A large-scale avalanche cycle is on-going.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1.5–3.5
    Wind slabs are failing on all aspects in the Alpine and at Treeline producing large to very large avalanches. Be aware of exposure to run-out zones. In many cases these avalanches are stepping down to the deeper buried weak layers.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1.5–3.5
    Several buried weak layers of concern exist down between 50 and 150cm. Loose dry slides or wind slabs initiated in the upper snowpack are often stepping down to these weak layers.

  • Loose Dry

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    1–2
    Ice climbers, avoid gullies. Expect sluffing in steeper terrain. Some sluffs are triggering slabs on the underlying slopes.

Confidence

High -

Weather Forecast

Tuesday will be mainly cloudy with isolated flurries. Ridge-top winds will be from the west at 25 km/h and a high of -13 C. Another storm will bring up to 25cm of new snow late Wednesday and into Thursday.

Avalanche Summary

A large-scale natural avalanche cycle occurred in the past 24hrs on all aspects in the Alpine up to size 3.5. A few slabs up to size 2.0 also initiated at Treeline. Smaller loose dry avalanches were widespread across all Treeline and Alpine terrain today. Explosives control work today on EEOR produced size 2.0 avalanches.

Snowpack Summary

Another 15cm of new snow brings recent storm snow totals to between 50 and 60cm. This has fallen with relatively little wind effect in the southern part of the forecast area, but more wind effect is evident up north. In the Alpine fresh wind slabs have formed on all aspects. A large natural avalanche cycle occurred over the last 24hrs associated with these fresh wind slabs. In some cases, avalanches stepped down to deeper weak layers such as the Jan 6 surface hoar and the Dec 15 surface hoar/sun crust/facet layer, producing large to very large avalanches. Forecasters continue to monitor multiple buried weak layers between 50 and 150cm down into the snowpack. In addition, the November crusts layers have recently become active in a few isolated avalanches in shallow snowpack areas.

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