Bollettino valanghe

Purcells

Dec 19 – 20, 2011Avalanche Canada
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Archiviato · scaduto 15 years ago

Pericolo valanghe

Wed
Thu
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–4
    Wind slabs are sliding easily on the recently buried surface hoar. Shifting winds have set up this problem on a variety of aspects, particularly north through south east.
  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–3
    Slab avalanches are now occurring on the mid-Dec surface hoar interface in northern parts of this region.

Avalanche Summary

Natural avalanches occurred in the Dogtooth range on Sunday up to size 2.0 at treeline on North through East aspects.

Confidence

Fair - Due to variable snopack conditions

Weather Forecast

Tuesday: Snow flurries with no significant accumulation expected. Strong NW ridgetop winds. Alpine temperatures falling rapidly to around -15C by the afternoon. Wednesday: Dry. Light to moderate northerly winds. Alpine temperatures around -16C. Thursday: Dry. Winds becoming westerly. Remaining cold, but a mild inversion should elevate alpine temperatures to around -10C.

Snowpack Summary

The Purcell region has been getting less snow in the recent storms than the Selkirks. This means in most areas we have not reached critical threshold on a layer of large surface hoar and near surface facets that was buried mid-December. An exception to this is in the Dogtooth range, where avalanches to size 2 have been releasing on this layer. In most areas the mid-December surface hoar layer currently lies about 20cm below the snow surface. Some areas have a sun crust in the alpine on steep south and west aspects. There is a rain crust that is buried between 40-55 cm in some areas that reaches up to about 2200 metres. Lower in the snowpack, the mid-layers are well-consolidated and strong. Near the base of the snowpack there are a few layers that have the potential to wake up with a really big storm or very heavy loads. These include a surface hoar layer from early November, a crust/facet combo from October and the interface on steep glaciated terrain with snow that did not melt over the summer.

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