Boletín de aludes

South Rockies

Feb 14 – 15, 2014Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

Sun
Mon
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
3 · Notable

Lo esencial

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Problemas de aludes

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    2–5
    The recent storm snow and wind have created a thick widespread slab which will be especially susceptible to human triggering on lee north and east aspects. Cornices have built up and may fall. Loose snow avalanches remain a concern.

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Tonight and Saturday: A trace of precipitation and clouds clearing tonight. Tomorrow cloudy with light southwesterly winds and the freezing level rising to 1100m. Alpine high -6.Sunday: Precipitation starting overnight and carrying into the day, accumulations of 5-10cm. Strong winds from the southwest at ridge tops. Alpine temperatures around -8. Monday: Mainly cloudy with accumulations to 5cm. Freezing levels around 1200m. Light southwesterly ridge top winds.

Avalanche Summary

On Wednesday a size 2 avalanche in the south eastern part of the region was triggered below treeline and caught and carried a skier. The slab was on a south east aspect, was 40 cm deep, and ran on on a combination of sun crust and facets beneath the storm snow. Several recent explosive, skier controlled, snowmobile triggered, natural avalanches and cornice falls sizes ranging from 1 to 2.5 have been reported on various aspects and elevations. Additional reports of "whumphing" settlements and shooting cracks from skis tips are highly indicative of an unstable snowpack.

Snowpack Summary

Over the last few days 30-50cm has been deposited across the region. South westerly winds have built reactive slabs 40- 80cm thick, on lee north and east aspects at upper elevations. Recent snowpack tests show sudden and easy results, indicating that storm slabs are not bonding well to underlying layers - these include; old hard slabs in the alpine, sun crusts, and several sandwiched layers of facets and surface hoar. The mid snowpack is strong and supportive. A deep persistent layer of facets and depth hoar near the base of the snowpack has remained dormant to this point, but may become a concern with additional load and stress on the snowpack.

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