Bulletin d’avalanche

Northwest Inland

Dec 16, 2017Avalanche Canada
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Archivé · expiré 9 years ago

Danger d’avalanche

Sun
Mon
Alpin
2 · Modéré
Limite forestière
2 · Modéré
Sous la limite
1 · Faible
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Points saillants

Slopes that are sheltered from the wind and sun  will likely offer the best riding.

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    1–2
    New wind slabs may be rider triggered. Watch for triggering in higher elevation, wind-exposed terrain.

  • Deep Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely - Possible
    Taille
    2–3
    The late October crust lies near the base of the snowpack with a thin layer of weak, sugary snow above it. This layer should be on a strengthening trend, but a heavy trigger in a thin snowpack area may still be enough to cause it to react.

Confidence

Moderate - Due to the number and quality of field observations

Weather Forecast

Saturday: Cloudy with sunny periods. Alpine temperatures -2 and freezing levels 1000 m. Ridgetop winds strong from the southwest.Sunday: Mix of sun and cloud. Alpine temperatures -3. Ridgetop winds light with strong gusts from the southwest.Monday: MIx of sun and cloud. Alpine temperatures -7. Ridgetop winds light from the southwest.Check out the Mountain Weather Forecast for more detail.

Avalanche Summary

No recent avalanche observations. Please submit your information to the Mountain Information Network. Give info get info.

Snowpack Summary

Snow surfaces are highly variable throughout the region. Solar and temperature crusts have formed on sun-exposed slopes, while stiff, stubborn wind slabs linger in leeward alpine terrain. Feathery surface hoar and surface facets have formed below treeline up to 1500 m. Approximately 30-50 cm of snow sits on two crusts that were buried near the end of November. These crusts are widespread and extend into the alpine. Although snowpack tests have previously shown hard results at these crust interfaces, more recent observations have been limited. Below these crusts, a well settled mid-pack overlies the late October crust near the base of the snowpack. This "crust/facet combo" layer is widespread and has not been reactive to rider and remote triggers since the end of November. These rain crusts will likely be with us all winter but may not pose a problem until we see a significant change in the weather.Average snowpack depths now total 80-140 cm at treeline elevations and up to 160 cm in the alpine.

Régions couvertes