Boletín de aludes

South Rockies

Dec 12 – 13, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

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

Continued strong ridgetop winds are driving the Danger Ratings in the alpine.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3
    Strong winds have developed stiff, touchy wind slabs at treeline and above. Cross-loaded slopes, gully features and loaded pillows in the immediate lee of slopes are most suspect and may be touchy to rider triggers.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–4
    Sugary facets near the base of the snowpack represent the most worrisome layer at this time. A surface hoar layer 30-40 cm down may be easily rider triggered with forecast new snow and warmer temperatures.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Saturday

Weather Forecast

Light snow is forecast overnight as the weakening cold front moves east from the coast. By Saturday another pacific frontal system will spread light amounts of precipitation accompanied by strong southwesterly ridgetop winds and gradual warming temperatures.Friday: Cloudy with sunny breaks and flurries. Alpine temperatures near -8. Ridgetop winds light from the SW. Saturday: Cloudy with snow amounts 5-10 cm. Alpine temperatures -6. Ridgetop winds strong from the SW.Sunday: Cloudy with snow amounts near 10 cm. Alpine temperatures -4. Ridgetop winds moderate from the SW.

Avalanche Summary

Explosives control saw a couple size 1.5 slab avalanches from NE-E aspects around 2000 m. I suspect that wind slabs may be easily rider triggered with the recent strong to extreme winds. Use extra caution on cross-loaded slopes, and in the immediate lee of ridgelines. Small loose dry avalanches are likely from steeper slopes, and do not support a significant problem unless you were pushed into a terrain trap like a cliff, or a gully.

Snowpack Summary

Incremental snowfall amounts have buried surface hoar crystals and a faceted upper snowpack. Snowpack depths at treeline seem to vary from 50 - 110 cm and widespread wind effect is noticeable in the alpine and at treeline.Down 30-40 cm sits a surface hoar/ facet/ crust interface. This layer seems to be less reactive to snowpack testing. However, with windy, warmer temperatures and new snow it may become more reactive as the slab above it develops.Near the base of the snowpack, weak sugary facets and depth hoar exist. This layer may be stubborn to trigger, especially in deeper snowpack areas. In shallower locations the likelihood may increase especially on a steep, convex slope. In some areas it is below threshold below treeline, and early season hazards like open creeks, and stumps exist.

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