Boletín de aludes

Kootenay Boundary

Feb 6 – 8, 2012Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Wed
Thu
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–6
    Forecast warm temperatures and strong solar radiation may weaken large fresh cornice growth. Cornice falls are a large load that may trigger deeply buried weak layers and cause large avalanches on the slopes below.
  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    3–7
    A couple of recent avalanches have released deep in the snowpack. Some may have stepped down from avalanches released due to warming on southerly aspects. Some others on north aspects may have failed on the deep weak layer with light triggers.

Confidence

Good - -1

Weather Forecast

A ridge of high pressure will continue to keep the region dry, and sunny through Tuesday. Ridgetop winds are light from the SE. Freezing levels near 1100m dropping to valley bottom overnight. The pattern will start to change on Wednesday afternoon. Light snow amounts are expected with freezing levels near 1200m. Alpine temperatures could drop to -9, and treeline temps may hover near -6. Light snow amounts may spread across the region on Thursday with freezing levels possibly reaching 1500m.

Avalanche Summary

One notable size 2 skier triggered avalanche occurred outside the ski area boundary near Whitewater. This was on a North aspect @1985m. The crown depth was reportedly 40-60cms, 50 wide and running 150m down slope. 2 skiers were involved, and sustained no injuries. Other observations from around the region includes small surface sluffing from steep North facing aspects.

Snowpack Summary

Temperatures dropped below freezing again Sunday night, and persisted through the day at higher elevations. Crusts have been forming due to the melt and freeze cycle for the past few days. There is still dry snow on northerly aspects at higher elevations. Sun crusts have developed on steep solar aspects. Pin-wheeling and other signs of moist snow have been observed on solar aspects at and above treeline At treeline and below treeline surface faceting and surface hoar growth (up to 15mm) are forming; especially on shady aspects in sheltered locations. This may become future layers of concern once buried. Steep planar slopes with shallow snowpacks are the most suspect. The recent storm snow layer is about 30-50 cm thick and is quite variable across the region. There are a couple of thin crusts buried below the storm snow that have been producing moderate to hard shears in tests. Some areas are still getting sudden planar shears on the mid-December surface hoar layer.

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