Boletín de aludes

South Rockies

Dec 8 – 9, 2012Avalanche Canada
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Archivado · caducó 14 years ago

Peligro de aludes

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

Lo esencial

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    New snow and winds have created new wind slabs. Watch for triggering in gullies, below ridgecrests and behind terrain features
  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–6
    We have not heard of any new releases on this early season rain crust; however, an avalanche at this interface could be surprisingly large and destructive.

Weather Forecast

Sunday: A short lived period of high pressure exists into midday Sunday. In the afternoon a weak upper trough approaches bringing cloudy skies, cooler temperatures, and moderate-strong West winds. Snow amounts 5-10 cm, alpine temps near -9, freezing levels at valley bottom.Monday: Trace of new snow, ridgetop winds NW 40-60 km/hr, alpine temps near -9, freezing levels valley bottom.Tuesday: Moderate snow fall amounts, ridgetop winds SW 30 km/hr, alpine temps near -8, freezing levels 1100 m in the afternoon falling to valley bottom overnight.

Avalanche Summary

No recent avalanche observations.

Confidence

Poor - Due to limited field observations for the entire period

Snowpack Summary

Recent storm accumulations have been variable throughout the region, however some ares saw significant snowfall earlier in the week. Recent accumulations may sit over a rain crust that extends up to 2000 m, the new snow may have a poor bond to this crust. Widespread wind slabs exist at higher elevations, although I suspect that in recent days they may have gained some strength. There have been reports of buried surface hoar up to a metre down. This layer, which was buried at the end of November, seems most prevalent on the west side of the region. Little is known about its current reactivity.At the base of the snowpack an early November crust which is associated with a layer of facets either directly above or below. Recent tests have shown sudden results at this interface. In general, snowpack data is sparse in this region and significant variations likely exist from one drainage to another. Digging down and making your own observations will be critical to safe slope selection. Any observations from the field are welcome at [email protected].

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