Bollettino valanghe

Northwest Coastal

Nov 23 – 24, 2011Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 15 years ago

Pericolo valanghe

Fri
Sat
Alta quota
4 · Forte
Limite del bosco
4 · Forte
Sotto il limite
3 · Marcato
Apri la mappa completa

In sintesi

Avalanche danger is expected to remain HIGH as long as the intense storms continue.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Very Likely
    Dimensione
    2–6
    I expect wind-loading will occur well below ridge crests and behind any terrain feature, especially in cross-loaded gullies. Large natural avalanches in response to heavy wind-loading are expected.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    1–4
    Storm slabs are likely very touchy, especially where they are sitting on surface hoar. Continued loading from new snow and rain will likely overburden weaknesses and cause natural avalanches.

Confidence

Poor - Due to limited field observationsfor the entire period

Weather Forecast

Thursday: 20-30cm of snow with freezing levels as high as 900m and extreme southerly winds becoming westerly late in the day.Friday: Light to moderate precipitation increasing intensity throughout the day with 10-20cm expected by the evening. Strong westerly winds becoming extreme southerlies. Freezing levels in valley bottoms in the morning rising to 900m throughout the day.Saturday: Heavy precipitation, extreme southwesterly winds and freezing levels as high as 1000m

Avalanche Summary

No recent avalanche have been reported, but I suspect natural avalanche activity occurred and will continue in response to heavy loading from snow and especially wind.

Snowpack Summary

Another 15cm last night keeps adding to the recent storm snow total, which is now probably 70-80cm since the weekend in some areas . Varying temperature, precipitation intensity, and wind throughout the recent storms, as well as surface hoar on the previous snow surface, has probably resulted in various weaknesses within upper snowpack. The mid and lower snowpack is generally well settled and strong with an old rain crust near the ground.

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