Boletín de aludes

Northwest Inland

Jan 23 – 24, 2016Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Mon
Tue
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil
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Lo esencial

Recent observations are very limited from the region. If you're out in the mountains please consider sharing your observations on the Mountain Information Network.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Watch for pockets of wind slab in exposed lee and cross-loaded terrain. These wind slabs could be triggered by the weight of a skier or sled, especially where they are sitting on a persistent weakness. 

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    New snow has been slowly accumulating over a layer of facets and surface hoar and may now be primed for triggering in some areas.

Confidence

Low - Due to the number of field observations

Weather Forecast

Sunday: Mainly cloudy. The freezing level is at valley bottom and winds are moderate from the southeast. Monday: Cloudy with light snow – around 5 cm. The freezing level could rise to 600-800 m and winds increase to strong from the S-SW. Tuesday: Periods of snow. The freezing level rises to 1000-1200 m. Winds remain strong from the southwest.

Avalanche Summary

There are very few observations from the region. A couple natural size 2 slab avalanches were observed in wind-loaded terrain (N-NE aspects) at around 1800 m on Friday.

Snowpack Summary

Light snowfall with moderate southeast winds may be enough to form fresh, reactive wind slabs in lee features. In some places this could also activate buried surface hoar in the upper snowpack, generally found between 30 and 60 cm deep. Stay tuned to signs of instability like recent avalanches, whumpfing, and shooting cracks. The mid pack that was reported to be well settled may have now facetted in the shallower areas, and the deeper basal layers are almost certainly facetted and weak. We have not heard of any full depth releases on weak basal layers yet.

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