Boletín de aludes

Kootenay Boundary

Jan 7 – 8, 2013Avalanche Canada
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Archivado · caducó 14 years ago

Peligro de aludes

Wed
Thu
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
2 · Moderado
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Lo esencial

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    New windslabs have formed in immediate lee and cross loaded locations. The forecasted winds are quite strong, meaning more intense slab development.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3
    I consider sluffing to be part of this problem. Where the storm snow is still shallow (less than 20cm) expect continued sluffing, but warming temperatures will promote settlement of deeper storm deposits into cohesive storm slabs.

Confidence

Fair - Intensity of incoming weather is uncertain

Weather Forecast

Tuesday: Cloudy, with precipitation building late in the day as a surface low approaches. Winds should be westerly 50-70km/h and freezing levels may climb to 1000m.Wednesday: The surface low should bring moderate to locally heavy snowfalls. Freezing levels may reach 1500m as the low advances with southwest winds reaching 60km/h.Thursday: The low should pass leaving occasional flurries and eventually sunny breaks. Winds turn northeasterly and diminish to 20km/h.

Avalanche Summary

Isolated windslabs in lee terrain to size 1.0 and continued sluffing in steep terrain to size 1.0.

Snowpack Summary

Up to 15cm of low density new snow has fallen recently. Moderate south/southwest winds have redistributed this new snow into small windslabs in immediate lee features in the alpine and exposed treeline.The January 4th interface consists predominantly of loose facets up to 30cm deep. In isolated locations (sheltered treeline and below treeline) surface hoar up to 12mm is present. There is a 1-3cm sun crust on steep south and west facing terrain. Above this interface is another surface hoar layer, creating a reactive sandwich of weak crystals. The storm snow is bonding poorly to this interface.The midpack is well bonded and strong. The November 28 surface hoar is still being found in isolated, sheltered below treeline locations buried 95-120cm. The deep crust/facet combo from early November still exists and concern remains (although unlikely) for triggering from a shallow spot.

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