Boletín de aludes

Sea To Sky

Nov 21 – 22, 2011Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Wed
Thu
Alta montaña
5 · Muy fuerte
Límite del bosque
5 · Muy fuerte
Bajo el límite
3 · Notable
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Lo esencial

This bulletin is based on limited data. Local variation in conditions and danger levels are 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
    Very Likely
    Tamaño
    2–5
    Near ridgecrests and terrain breaks, and in cross-loaded gullies. Heavy wind-loading is expected to cause widespread large avalanche activity.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    3–6
    Particularly touchy where there is an associated rain crust, which is prominent between 1800m and 2050m.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    1–4
    Heavy loading from snow and rain is expected to cause widespread avalanche activity, particularly in immediate coastal areas.

Confidence

Fair - Due to limited field observationsfor the entire period

Weather Forecast

Very heavy precipitation is expected overnight Monday into Tuesday, with over 100mm for coastal areas, before easing Tuesday Afternoon. Winds are expected to be strong to extreme southwesterlies during the height of the storm and freezing levels generally around 1500m could briefly rise as high as 1700m.Wednesday: Another 20-40cm of snow expected with freezing levels dropping down to 1000m and strong southwesterly winds.Thursday: Continued moderate to heavy precipitation with associated strong southwesterly winds, especially for coastal areas.

Avalanche Summary

I suspect widespread natural avalanche activity will occur overnight Monday into Tuesday during the height of the storm. Large avalanches from alpine and treeline elevations could run well below treeline.

Snowpack Summary

Newly formed surface hoar is now buried in many locations, particularly sheltered open treeline slopes. A rain crust with associated facets is generally down 50-80cm also has surface hoar crystals sitting on top and/or slightly below it. A deeper crust with associated facets and/or depth hoar is approximately 50cm off the ground. Recent snowpack tests on a northeast facing treeline slope gave moderate sudden results on both of these weaknesses.

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