Bulletin d’avalanche

Northwest Inland

Feb 22 – 23, 2017Avalanche Canada
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Archivé · expiré 10 years ago

Danger d’avalanche

Thu
Fri
Alpin
2 · Modéré
Limite forestière
2 · Modéré
Sous la limite
1 · Faible
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Points saillants

Changing wind directions may develop new wind slabs on Thursday.

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    1–2
    Changing wind directions may develop new wind slabs on south through west aspects. Old wind slabs may continue to linger on other aspects.

  • Deep Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely - Possible
    Taille
    2–4
    A weakness at the bottom of the snowpack is lingering and may be triggered in shallow snowpack areas or by the weight of smaller avalanches.

Confidence

High -

Weather Forecast

Tonight: Mostly clear with moderate northerly winds and alpine temperatures around -15. Thursday: Mix of sun and cloud with strong northerly outflow winds and alpine temperatures around -17. Friday: Clear with strong northeast outflow winds and alpine temperatures around -15. Saturday: Overcast with flurries or light snow and moderate to strong northwest winds.

Avalanche Summary

Report on Tuesday of a size 2.0 avalanche on the "5000" run off Hudson Bay Mountain in Smithers. This was a visual report from town, the sliding surface is unknown but suspected to be the recent storm snow.

Snowpack Summary

10-15 cm of recent storm snow has been transported by the wind, and now sits on a variety of old surface conditions including isolated wind slabs, pockets of soft snow (5-10 cm deep), sun crusts, and surface hoar. A supportive rain crust exists below 1000 m. A layer of surface hoar that was buried on February 10th may exist 30-60 cm below the surface, but there's a fair bit of uncertainty regarding the reactivity and distribution of this layer. A stiff mid pack sits above weak sugary snow near the ground. Although possibly dormant, this basal weakness has the potential to produce very large destructive avalanches.

Régions couvertes