Boletín de aludes

Northwest Inland

Nov 24 – 25, 2015Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Thu
Fri
Alta montaña
Sin grado
Límite del bosque
Sin grado
Bajo el límite
Sin grado

Lo esencial

The snowpack is extremely variable depending on aspect and elevation. Stiff wind slabs with wide propagations may be ripe for rider triggering. Check out the Mountain Information Network. Give info, get info!

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–3
    Watch for new wind slabs on opposite slopes due to changing winds from the north. Last weekend's storm may have formed reactive wind slabs at higher elevations. Watch for wide propagations, especially in the lee of ridgecrests.

Weather Forecast

The arctic high remains stationary over the north giving cool and dry conditions on Wednesday. Treeline temperatures will hover near -12 with light winds from the northerly quadrants. Late Wednesday, warm air aloft will start to invade the coastal regions allowing temperatures to rise anywhere from 0-5 degrees between 1100-2500 m. Ridgetop winds will also change, blowing light from the southwest well into the weekend.

Avalanche Summary

No new avalanches have been reported. Newly formed wind slabs may remain sensitive to human triggering for the next few days, especially in areas with buried persistent weak layers.

Snowpack Summary

The snowpack is extremely variable depending on aspect and elevation. I suspect new wind slabs developing on reverse loaded southerly slopes and widespread surface crusts at lower elevations. At upper elevations, last weekends storm likely produced stiff wind slabs on northerly aspects. The reactivity of these new wind slabs will likely change with elevation and underlying snowpack structure. Due to limited observations, I have very little confidence in what that underlying structure may be, although I suspect faceting, crusts and surface hoar may exist. However; how are they adjusting and reacting as shears? Are they visually distinct and reacting like a cash register when tested? Or are they becoming hard to find with a more resistant shear characteristic? If I were traveling in the mountains, I'd maintain an investigative approach and dig down to test for weak layers before committing to a slope.

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