Boletín de aludes

Northwest Coastal

Jan 7 – 8, 2016Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Sat
Sun
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Outflow winds may have developed new wind slabs at all elevations. New wind slabs may be sitting on a weak layer of surface hoar or sun crust that can act as an easy sliding layer.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Strong outflow winds continue to build wind slabs. Outflow winds have been strongest in areas near the coast and adjacent to large low level valleys.

Confidence

Moderate - Wind effect is extremely variable

Weather Forecast

On Friday the region will see mainly sunny skies and light ridgetop winds, although areas closer to the coast may see strong outflow winds. Saturday will bring mainly overcast skies, up to 5cm of new snow and strong southwest winds as a Pacific front brushes up along the North Coast. On Sunday, expect a mix of sun and cloud and reduced winds. Freezing levels are expect to remain at valley bottom for all 3 days.

Avalanche Summary

Some recent natural wind slab activity to size 2.0 was reported from the north of the region near the coast where the outflow winds were reported to be strong. There have been no reports of avalanches from the ski operations in the south or from MIN reports.

Snowpack Summary

Snowpack surfaces are highly variable. A melt-freeze crust can be found at or near the surface on steep, solar aspects in the alpine. On most other slopes, 25-40 cm of snow from the Boxing Day storm continues to settle and facet, and new surface hoar has been reported although its distribution is likely variable due to strong outflow winds. In areas where recent winds have been light, shaded slopes will likely provide settled powder. In areas where winds have been stronger, reactive wind slabs may exist, especially in areas where the the slab overlies surface hoar buried by the Boxing Day storm. Professionals in the region are still tracking a few other surface hoar layers that developed throughout December which are now buried in the top 100cm. These layers have likely gained significant strength, and represent a low probability / higher consequence scenario at treeline and below treeline elevations. In colder and shallower snowpack areas watch for weak basal facets.

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