Boletín de aludes

Northwest Coastal

Feb 5 – 6, 2015Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Sat
Sun
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
4 · Fuerte
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Lo esencial

Extreme wind and heavy snowfall should ramp up Thursday evening. Only the most conservative non-avalanche terrain is appropriate this weekend.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    3–6
    This storm system should be a good test for the more deeply buried weak layers. With up to a meter of new snow expected in the alpine by Saturday afternoon, I wouldn't be surprised to see storm slabs step down to one of the persistent weaknesses.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1–5
    Significant snowfall and extreme winds are expected to drive a large natural avalanche cycle that will likely last through Saturday. Probably best to stay out of avalanche terrain while the storm is raging.

Confidence

Fair

Weather Forecast

Extreme southerly winds in the alpine along with strong east through south winds below treeline are expected through the forecast period. The freezing level should stay right around 600m and a few significant shots of precipitation are expected. 10 to 40 cm are possible Thursday night, another 10 to 40cm are expected Friday with 5 to 25cm on tap for Friday night. Fore a more detailed look at this dynamic weather pattern visit avalanche.ca/weather

Avalanche Summary

On Wednesday, (before the storm) a size 2.5 wind slab avalanche was reported from a steep SE facing feature at 1300m. I suspect there will be more activity to report on in the next few days.

Snowpack Summary

35- 60cm of new snow has fallen in the last few days. Strong winds have redistributed this snow in exposed terrain forming winds slabs in leeward features and stripping exposed slopes. The late-January crust is typically down 100-140cm in the south of the region and about half this depth in the north. Tests are indicating that this interface is generally well bonded but isolated avalanches have been reported to have released on this layer recently. The mid-January rain crust and/or surface hoar layer is down over 150cm in the south and has generally become inactive. It may still be a concern in thinner snowpack areas. The November crust/facet combo near the bottom of the snowpack is thought to be generally well bonded. However, this deep and destructive layer is still reported to be reactive in the far north of the region.

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