Boletín de aludes

South Rockies

Dec 16 – 17, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

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

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Wind slabs have developed recently on a variety of aspects due to shifting winds. Expect to encounter these deep deposits of wind-transported snow below ridge crests and behind terrain features.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–4
    Sugary facets at or near the base of the snowpack are most likely triggered on steep, convex slopes with a thin snowpack. In deeper snowpack areas you may find a stubborn buried surface hoar layer.

Confidence

Fair - Due to the number of field observations

Weather Forecast

On Tuesday, a low pressure system will move across central BC. While the system is expected to miss the South Rockies, the associated warm front will cause freezing levels to rise even higher, up to around 2300m. A weak ridge of high pressure will build after the low passes. The associated cold front on Wednesday will bring light snowfall to the region. Another low pressure system is expected to hit the coast on Thursday.Tuesday: A mix of sun and cloud, freezing levels as high as 2300m, moderate westerly alpine windsWednesday: Light snowfall, freezing levels dropping to valley bottom, light SW winds switching to NE during the dayThursday: A mix of sun and cloud, light NE winds switching to SW during the day

Avalanche Summary

No new avalanches reported.

Snowpack Summary

Recent incremental snowfall has started to bury the mid-Dec surface hoar and the previously faceted upper snowpack. Snowpack depths at treeline seem to vary from 50 - 110 cm with high variability in wind-exposed areas. Buried surface hoar/facets/crust (late-Nov interface) are down approximately 30-40cm. The base of the snowpack is made up of weak facets and depth hoar. This deep persistent weakness may be stubborn to trigger, especially in deeper snowpack areas, but the sensitivity to triggers likely increases in shallower locations, especially on a steep, convex slopes. In some below treeline areas the snowpack is below threshold and early season hazards like open creeks and stumps remain a concern.

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