Boletín de aludes

Purcells

Dec 15 – 16, 2014Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Wed
Thu
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil
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Lo esencial

A deeply buried weak layer is still producing large destructive avalanches in isolated areas and may be remotely triggered from a distance.  Use extra caution around steep, unsupported alpine terrain.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    Strong southerly winds last week created wind slabs in the alpine. Triggering these slabs has become more stubborn but they remain a concern, especially in steep, unsupported terrain.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–5
    The likelihood of triggering a persistent slab has decreased but the consequences remain very high. Be wary of any slopes that did not release during the storms. Remote triggering of this layer may also be possible.

Confidence

Fair - Due to the number of field observations

Weather Forecast

High pressure persists over the interior for the forecast period. A mix of sun and cloud is expected on Tuesday with treeline temperatures around -8 and light alpine winds. Wednesday and Thursday may see an increase in cloud cover while treeline temperatures should remain around -8 and alpine winds should remain light.

Avalanche Summary

On Monday, explosive control produced a size 3 deep slab avalanche.  A report on Sunday of a skier remotely triggering a size 2.5 avalanche from 5 meters away in the Dogtooth range alpine. This occurred at around 2300m in the alpine. Also reported was an explosive triggered size 2 persistent slab releasing around 60cm deep.

Snowpack Summary

A surface crust exists up to around 2200 m. Above this elevation is dry storm snow which is settling out and faceting. A new layer of surface hoar is currently forming on the snow surface. In exposed alpine terrain, strong southerly winds last week may have resulted in variable distribution of the surface snow and the formation of wind slabs. The early November crust/facet layer is down around 1 m. Tests are suggesting that this layer is getting difficult to trigger but still has the potential to produce large avalanches.  We received reports that this deep weak layer has resulted in remotely triggered avalanches over the weekend.

Regiones cubiertas