Boletín de aludes

South Coast

Nov 22 – 23, 2015Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Tue
Wed
Alta montaña
Sin grado
Límite del bosque
Sin grado
Bajo el límite
Sin grado

Lo esencial

Given the very limited information on hand for this bulletin, I would tread cautiously and take the time to gather snowpack information as I go. As always, we would love for you to submit any observations from your day to the MIN.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1–2
    New snow and wind will cause the Avalanche Danger to rise throughout the day on Monday. Watch for new wind slabs in the lee of ridgecrests and terrain breaks.

Confidence

Poor - Due to the number of field observations

Weather Forecast

On Monday, a fast-moving Pacific frontal system will bring 5-15cm of new snow, moderate southwest winds and freezing levels at about 500m. Expect a clearing trend on Tuesday and Wednesday as a dry ridge of high pressure sets up over the region. Ridgetop winds associated with the ridge should remain northeasterly, blowing up to 60kmh on Tuesday, then easing somewhat on Wednesday. Freezing levels on Tuesday and Wednesday should hover around valley bottom.

Avalanche Summary

No recent avalanches have been reported. New snow and wind forecast for Monday will likely promote a fresh round of wind slab avalanche activity.

Snowpack Summary

Snow depths are highly variable across the region; however, slopes below treeline are still below threshold for avalanche activity. A dusting of loose snow overlies a widespread rain crust that is reported to exist up to about 2100m in many parts of the region. A Mountain Information Network report near the Coquihalla Highway also indicated well-developed surface hoar above the crust. New snow forecast for Monday may bond poorly to this potentially weak surface structure. Where the near-surface crust is robust (>1cm thick), the upper snowpack has gained strength and avalanches failing on deeper layers have become much less likely. I'd be extra cautious in areas where the near-surface crust is thin or has not formed (I'm thinking high alpine terrain or northern parts of the region). In these areas, deeper persistent weak layers may still be sensitive to human triggering.

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