Boletín de aludes

Purcells

Nov 15 – 16, 2011Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

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

This bulletin is based on limited data. Local variation in conditions and danger levels is likely to exist. To produce more accurate forecasts, we need information. Please send an email to [email protected].

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    Strong southerly, then north-westerly, winds have shifted snow onto downwind slopes.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Over the last two days, widespread storm slab activity has been observed. Weak snow at the base of the snowpack is likely to take time to gain strength. Steep or exposed terrain should be treated with suspicion.

Confidence

Poor - Due to limited field observations

Weather Forecast

Skies are briefly clearing ahead of the next band of precipitation, which is due to arrive late on Wednesday. Light snowfall is expected overnight Wednesday and on Thursday morning. Temperatures should remain cool.There is a chance of another pulse of snow arriving on Friday but weather models are showing uncertainty.

Avalanche Summary

A cycle of natural avalanche activity was observed in Quartz Creek on Sunday. Wind slabs (20cm deep) and persistent slabs (60cm deep) were observed. Persistent slabs were propagating widely and running on a weakness towards the base of the snowpack. Observations are limited to the northern Purcells.

Snowpack Summary

There is significant variability in the snowpack across the region. Snowpack depth at treeline varies from around 40-130cm. Up to 50cm of snow fell over the last few days, which was redistributed by strong winds blowing first from the south and then from the north-west. A basal layer of facets was reported in the Dogtooth Range, with a weak interface between the lower facets and recent storm snow. Observations are limited.

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