Boletín de aludes

Northwest Coastal

Jan 8, 2017Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

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

Increasing outflow winds will transport new snow and maintain dangerous avalanche conditions.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–3
    Weak layers of buried surface hoar up to a metre deep may be reactive after the recent loading. Take extra care to avoid thin trigger points and exposure to overhead hazard.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–2
    Strong outflow winds will continue to build touchy slabs that sit above a variety of weak layers including surface hoar.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

SUNDAY: Sunny, moderate east winds increasing to strong overnight, alpine temperatures around -15.MONDAY: Cloudy with scattered flurries and accumulations of 5 cm, strong outflow (east) winds, alpine temperatures around -10.TUESDAY: Sunny, strong to extreme outflow (east) winds, alpine temperatures around -15.

Avalanche Summary

On Saturday, poor visibility limited avalanche reports to a few size 1 natural avalanches at low elevations, but larger storm slab avalanches likely occurred at higher elevations. Large persistent slab avalanches have been reported on a regular basis in the Ningunsaw area for the past few weeks.On Sunday, increasing winds will transport the recent storm snow and continue to build touchy storms slabs. Triggering larger persistent slab avalanches on buried surface hoar layers remains possible.

Snowpack Summary

20-50 cm of new storm snow sits above a variable interface composed of hard wind slabs, weak surface hoar, and faceted snow. Expect the new snow to bond poorly to this interface and form extra touchy storm slabs on wind-loaded features. Wind-loading will likely occur on a wide variety of aspects, as winds are shifting to the northeast. Below the new snow, a well settled slab sits above the Christmas surface hoar layer, which is now buried 50-100 cm deep and may still be reactive in sheltered areas. Deeper weak layers have only been reactive in areas with thin snowpacks. This includes a facet layer from mid-December that has been reactive in snowpack tests at lower elevations, and weak facets near the ground that have produced avalanches in the northern part of the region.

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