Boletín de aludes

Northwest Inland

Mar 11 – 12, 2012Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Tue
Wed
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
2 · Moderado
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Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    Forecast strong winds and new snowfall will continue to form fresh wind slabs, generally below ridgecrests, behind terrain features and in gullies. Cornices are also large and weak, and could trigger wind slabs on the slope below.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    3–6
    The persistent weak layer that formed in early February continues to be buried by a few cm each day. Avalanches on this layer have not been reported for a few days, but we feel that it could still be triggered by skiers and riders.

Confidence

Fair - Due to limited field observations

Weather Forecast

Monday: Up to 10cm of new snow - moderate to strong easterly winds - freezing level at surface Tuesday: Light snowfall - light to moderate southwesterly winds - freezing level at surface Wednesday: Light snowfall - moderate southeast winds - freezing level rising to 600m

Avalanche Summary

No new avalanches to report. We'd love to hear about what you've seen in the field. Any observations can be sent to: [email protected].

Snowpack Summary

Warm temperatures and then subsequent cooling have created crusts on all aspects below 1000m and on sun-exposed slopes as high as 1600m. More recently, intense wind-loading and light snowfall accumulations have taken place with snow surfaces either getting scoured or packed into hard wind slabs. The mid February interface, down around 60cm, is variable and generally consists of a strong melt freeze crust below 1000m. Above that elevation, expect to find buried facets, and/or surface hoar (in more sheltered areas), and/or a sun crust on southern aspects. The surface hoar is not widespread, but has been responsible for larger avalanches that occurred last week. This layer should be on your radar, as it may be susceptible to rider triggers.

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