Bulletin d’avalanche

Purcells

Dec 26 – 27, 2013Avalanche Canada
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Archivé · expiré 13 years ago

Danger d’avalanche

Sat
Sun
Alpin
3 · Marqué
Limite forestière
3 · Marqué
Sous la limite
2 · Modéré

Points saillants

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible - Likely
    Taille
    1–3
    Moderate to strong west and southwest winds creating new windslabs in the lee of terrain features. A small wind slab release may be enough to trigger a deep weak layer, producing a large and destructive avalanche.
  • Deep Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    2–5
    The sensitivity to triggers is increased in shallow locations, especially on steep, convex, north-facing slopes.

Avalanche Summary

The deep persistent slab problem continues to be reactive up to size 3 with larger triggers such as explosives. Rider triggering is possible especially in shallow snowpack areas like rocky outcrops or near small trees.

Weather Forecast

Friday: Light precipitation. Alpine temperatures -2. Moderate to strong southwesterly winds switching to northwest in the afternoon. Freezing level 1500mSaturday: Mainly dry with broken skies, winds moderate to strong from the northwest and alpine temperatures -7.Sunday: Light snowfall, alpine temperatures -9, winds light to moderate from the northwest.

Confidence

Fair - Track of incoming weather systems is uncertain on Friday

Snowpack Summary

Up to 25 cm of new storm snow covers stiff, dense wind slabs in exposed lee terrain at and above treeline. Average snowpack depths at treeline elevations are 100-130 cm. In the upper 80 cm of the snowpack a couple persistent weak layers exist, comprising of surface hoar and a facet/crust combo. This interface has produced variable results with snowpack tests, and operators are keeping a close eye on them as the load above increases and/or a slab develops.A bigger concern, especially in the Northern part of the region where the snowpack is thinner and more variable is weak faceted and depth hoar crystals combined with a crust from early October. This is now down around 80-120 cm. This deep persistent weakness may be stubborn to trigger, especially in deeper snowpack areas, but the sensitivity to triggers likely increases in shallower locations, especially on steep, convex, north-facing slopes.

Régions couvertes