Boletín de aludes

South Coast

Dec 21 – 22, 2014Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Tue
Wed
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

There may be a lot of variability between the North and South areas of this region. Time to dig down and find out what the snowpack looks like in your area, and then share your observations with us!

Problemas de aludes

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–3
    The recent storm slab is expected to take a few days to settle and bond to the old surfaces. Some deep pockets of windslab may exist in the alpine and at treeline on terrain that is in the lee of Southwest winds.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    3–5
    The increasing load of new storm snow may increase the likelihood of triggering the deeply buried weak crust layer.

Confidence

Poor - Due to the number of field observations

Weather Forecast

Flurries or light snow overnight combined with strong Westerly winds and dropping freezing levels. Drier and cooler on Monday with periods of broken skies with light Westerly winds. The next storm should move into the region sometime early on Tuesday morning and bring 5-10 cm during the day with strong Southwest winds. The storm should continue overnight and into Wednesday morning, but at this time the snowfall amounts look very light.

Avalanche Summary

Soft slab avalanches were reported during the storm from alpine North aspects up to size 1.5 on Saturday. I suspect that storm slab avalanches continued on Sunday with the additional 20-25 cm of new snow combined with strong winds.

Snowpack Summary

The new storm slab may be 40-50 cm thick in The Coquihalla and is reported to be bonding well to the December 11th crust. In the Coquihalla there is 70-100 cm of snow on the ground above 1600 metres elevation, and below threshold for avalanches below 1500 metres. The recent surface hoar has been reported to have been mostly blown away by the Northeast wind before this new storm. In the North of the region it sounds like the recent surface hoar is 2-4 mm at treeline and up to 30 mm near open creeks below treeline. The knife hard December melt-freeze crust extends up to about 2100 metres and then tapers off to nothing by 2300 metres. The new storm slab may be up to 70 cm in the North of the region, and it may not be bonding well to the old crust/ surface hoar combination. The November crust is deeply buried and may become easier to trigger in isolated areas if the load from the storm slab overcomes the bond at the crust interface.

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