Boletín de aludes

South Columbia

Nov 23 – 24, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

Mon
Tue
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil
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Lo esencial

Forecast produced with limited field observations.  If you're in the field, please send any information to:[email protected]

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–4
    Wind slabs persist in the alpine and at tree line especially on lee slopes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–5
    A crust layer buried near the base of the snowpack will remain problematic for some time to come, with the possibility of producing large and destructive avalanches.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    Rising temperatures can produce wet sloughs on southerly aspects and may trigger deeper instabilities

Snowpack Summary

Recent storm snow is settling and will gain strength with time and warming temps. Wind slabs linger in lee terrain. Surface hoar buried in early November exists in the mid snowpack but due to a lack of data little is known about its reactivity. The October crust/facet interface buried in the lower snowpack will likely be of concern for the foreseeable future. Valley fog and cold clear temps are producing a new surface hoar layer at fog levels and in sheltered north aspects.

Confidence

Fair - Due to the number and quality of field observations

Weather Forecast

Cool temps will give way to gradual warming for the forecast period with freezing levels going up to 3000 M in the next few days. No significant precipitation is in the forecast for the next 7 days. Winds are expected to be generally light to moderate for the forecast period.

Avalanche Summary

High winds accompanying the last significant snowfall produced wind slabs in exposed alpine and tree line locations producing avalanches up to size 3. Rising temps may produce wet sloughs on steep S facing alpine slopes and could trigger deeper instabilities

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