Boletín de aludes

Purcells

Feb 19 – 20, 2013Avalanche Canada
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Archivado · caducó 14 years ago

Peligro de aludes

Thu
Fri
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
2 · Moderado
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Lo esencial

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–5
    There are a couple of older layers of buried surface hoar and crust combinations that are buried down about 70 cms and 100 cms, that may be triggered by large additional loads.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    The buried February 12th surface hoar layer is expected to continue to be reactive. The amount of snow above the weak layer is variable across the region. Watch for increased reactivity with exposure to direct sunlight.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Wednesday: Mix of sun and cloud / Light northwest winds / Freezing level at 900mThursday: Very light snowfall intensifying in the evening / Moderate west winds / Freezing level at 800mFriday: Moderate snowfall / Light to moderate southwest winds / Freezing level at 1000m

Avalanche Summary

On Monday a size 2 skier-triggered avalanche occurred near Invermere which resulted in a fatality. The avalanche ran on a south/southeast aspect at 2700m and is thought to have failed at the February 11/12 interface.

Snowpack Summary

Very light amounts of low density snow add to the recently developed storm slab that is between 15-60 cms across the region. The recent storm slab is expected to remain reactive where it is sitting on the weak surface hoar layer that was buried on February 12th. The recent storm slab has also been reactive on Southerly aspects where a sun crust formed during the period from February 8th-11th. Solar radiation or future loading may cause another cycle of natural activity, or an increased sensitivity to human triggers. There are older weak layers that are now buried down around 70-80 cms, and also at about 110 cms. These layers have been less likely to trigger by skiers, but they may still be sensitive to large loads like avalanches in motion or cornice fall.

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