Boletín de aludes

South Rockies

Nov 24 – 25, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

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

Please note this bulletin is based on very limited information. If you have been out and have observations, please send them to [email protected].

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    This problem is likely a thing of the past, but be aware that it may still be a concern on steep slopes in the alpine that did not slide previously.

Confidence

Poor - Due to the number of field observations

Weather Forecast

Synopsis: The current pattern remains in place through Tuesday. On Wednesday a weak frontal system should clear out the inversion. No significant change in the weather for the forecast period.Monday: Freezing Level: Near 0 C at Valley Bottom, above freezing layer from 1500 2500m. Precip: No significant precip expected. Wind: Light, Variable.Tuesday: Freezing Level: Near 0 C at Valley Bottom, above freezing layer from 1500 2500m. Precip: No significant precip expected. Wind: Light SWWednesday: Freezing Level: 1200m Precip: No significant precip expected. Wind: Light, SW.

Avalanche Summary

Avalanche activity was reported in pockets of deeper snow from Monday (18th) and Tuesday (19th) in both western and eastern areas of the region. Activity appears to have tapered off.

Snowpack Summary

Observations from this region are extremely limited at the moment.Winds have wreaked havoc on much of the region leaving behind old tired windslabs and plenty of wind damaged snow.  Treeline snowpack depths in sheltered areas vary between approximately 40-80 cm. In the alpine, coverage is highly variable due to recent high winds. A crust or significant density change may exist around 40 cm below the surface. This has been reported to have weak faceted crystals above and below, and produces sudden "pop" results in compression tests. Below this near the base of the snowpack, an earlier crust buried in October lies close to the ground. This layer may still be of concern on isolated smooth terrain features that have not seen avalanche activity.

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