Boletín de aludes

Purcells

Apr 17 – 18, 2014Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Sat
Sun
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

Avalanche danger can rise very quickly with warming temperatures and/or brief periods of sun. Be aware of changing conditions and overhead hazards.For more insight into spring danger ratings, check out our Blog Post.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    New wind slabs  immediately lee of ridge crest may be sensitive to human triggering.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Expect to see an increase in avalanche activity with forecast rain at lower elevations or on solar aspects if the sun comes out for extended periods of time.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    4–8
    The potential for very large deep slab avalanches needs to remain on your radar. Cornice fall, strong sun, warming temperatures or a surface avalanche in motion could act as triggers.

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Tonight and Friday: Flurries (total accumulation: 5-10cm) / Light westerly winds / Freezing level 1800mSaturday: Cloudy with sunny periods and isolated flurries  / Light westerly winds  / Freezing level 2000.Sunday:  Flurries (total accumulation: 5-10cm) / Light westerly winds / Freezing level 2000m

Avalanche Summary

There have been no new avalanche observation

Snowpack Summary

A recently buried, supportive crust can be found near the surface of the snowpack on all aspects and elevations except for high elevation north-facing terrain.Three persistent weak layers still exist in the highly variable snowpack of the Purcells: The mid-March sun crust/surface hoar layer down 50-80cm and the early-March crust/facet/surface hoar layer down around 80-120cm seem to be laying dormant for the time being. The mid-February crust/facet/surface hoar combo is typically down 60 - 120cm. Direct triggering of this layer has become unlikely, however, cornice fall, a smaller avalanche in motion or prolonged warming may wake this layer up.  The resulting avalanche would be very large and destructive.At the base of the snowpack weak basal facets can be found in many areas, however triggering this layer is unlikely

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