Bulletin d’avalanche

Purcells

Feb 19 – 20, 2012Avalanche Canada
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Archivé · expiré 15 years ago

Danger d’avalanche

Tue
Wed
Alpin
2 · Modéré
Limite forestière
2 · Modéré
Sous la limite
1 · Faible
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Points saillants

Check out the recent Forecaster Blog post discussing the "Tipping Point".

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    1–4
    Fri/Sat winds were out of the S, SW, Sun.out of the NW. This combination has set up thin wind slabs behind exposed terrain features.

  • Deep Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely
    Taille
    3–7
    Although a deep persistent slab would most likely require a large trigger (such as cornice fall), they are still possible; especially in thin snowpack areas or in unsupported, rocky terrain.

Confidence

Fair - Intensity of incoming weather is uncertain on Tuesday

Weather Forecast

Monday and Tuesday: flurries both days bringing minimal accumulation of new snow. Light to moderate NW winds increasing to strong NW on Tuesday. Freezing level around 800 m. Tuesday night into Wednesday: a slightly stronger band of moisture arrives bringing around 10 cm new snow, freezing levels rising to 1800 m and strong westerly winds.

Avalanche Summary

On Saturday, small avalanches could be triggered in the top 20 cm of snow by ski cutting. As we get incremental amounts of new snow above this interface, we inch closer to the tipping point, when more widespread and dangerous avalanches start to occur. This concept is discussed in more detail in the latest Forecaster Blog post.

Snowpack Summary

Widespread surface hoar has been buried by around 10 cm of new snow in most of the region. The exception is terrain closer to the Bugaboos, where the interface is down 20-40cm. A melt-freeze is also associated with this weak interface on southerly aspects at all elevations. North and east aspects continue to have dry snow and some surface sloughing in steep terrain. Basal facets have not been reactive, but operators continue to monitor this layer in tests. Triggering this deep persistent weak layer is unlikely, but shallow snowpack areas or shallow weak areas adjacent to deeper wind loaded slopes are suspect locations.

Régions couvertes