Bulletin d’avalanche

South Columbia

Dec 1 – 2, 2013Avalanche Canada
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Archivé · expiré 13 years ago

Danger d’avalanche

Tue
Wed
Alpin
4 · Fort
Limite forestière
3 · Marqué
Sous la limite
2 · Modéré
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Points saillants

Recent snowfall amounts have been highly variable throughout the region. In some areas (particularly the Monashees where accumulations were reported to be the highest), Treeline and Below Treeline danger ratings may be higher than posted.

Problèmes avalancheux

  • Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely - Possible
    Taille
    3–5
    Loading from the recent storm may reactivate persistent weaknesses buried in the mid and lower snowpack. If triggered, avalanches on these layers would be large and destructive.

  • Storm Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely - Very Likely
    Taille
    1–5
    Touchy storm slabs exist with the potential to create large avalanches. Storm slabs may be more reactive on slopes affected by wind, or in areas where they overlie surface hoar. Sluffing may also occur where new snow is unconsolidated.

Confidence

Good

Weather Forecast

Monday: A mix of sun and cloud with the possibility of light flurries / Light northeast winds / Alpine temperature of -10.0Tuesday: Clear skies / Light north winds / Ridgetop temperature of -18.0Wednesday: Clear skies / Light winds / Ridgetop temperature of -18.0

Avalanche Summary

No reports of recent avalanche activity have been received. This likely speaks more to the lack of observations rather than actual conditions.

Snowpack Summary

Recent storm accumulations have been highly variable throughout the region with roughly 30cm falling in the Selkirks and close to double that in some parts of the Monashees. This new storm slab will increase in reactivity and destructive potential as it deepens or in areas where it has been redistributed and compressed by wind. The new snow covers a variety of old surfaces which include: old wind slabs at higher elevations, melt-freeze crusts on previously sun-exposed slopes and touchy surface hoar in sheltered terrain.In the mid snowpack you may find a layer of surface hoar buried in mid-November ranging from 90cm-130cm in depth. An October crust/facet combo exists near the base of the snowpack. The most likely place you'd trigger this layer is on smooth, planar, high north facing slopes, especially if the snowpack is unusually shallow in that area.These persistent layers are slowly becoming more difficult to trigger. However, they have the potential to cause large and destructive avalanches, and may 'wake-up' with the increased load of the new snow.

Régions couvertes