Boletín de aludes

Northwest Inland

Mar 18, 2017Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

Sun
Mon
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Sustained and shifting winds are driving a wind slab problem at higher elevations. The potential for a wind slab release to trigger a deeper persistent slab can't be overlooked.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2
    Moderate to strong winds have shifted from southeast to southwest, leaving fresh wind slabs on a wide range of aspects. Use increasing caution as you enter wind affected terrain, especially in the lee of exposed terrain features at treeline and above
  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–3
    A lingering weakness at the bottom of the snowpack is here to stay. It will be most reactive in thin rocky start zones and in shallow snowpack locations.

Confidence

High -

Weather Forecast

Saturday: A mix of sun and cloud with isolated flurries and a trace of new snow. Light southwest winds. Alpine temperatures of -9. Sunday: A mix of sun and cloud with isolated flurries and a trace of new snow. Moderate to strong southwest winds. Alpine temperatures of -8. Monday: Cloudy with sunny periods. Light southeast winds. Freezing level rising to 1000 metres with alpine temperatures of -7.

Avalanche Summary

No new avalanches have been reported, but a report from the north of the region detailed a remotely triggered Size 2 storm slab releasing on a northeast aspect at 1400 metres on Wednesday. The slab depth was 50 cm. Numerous natural avalanches up to size 2.5 were reported from the west of the region in the Howsons on Tuesday. Natural avalanches up to size 2.0 were reported from the Hankin area on Monday.

Snowpack Summary

At treeline and above, ongoing winds have been redistributing recent storm snow and light new snow amounts into wind slabs in lee terrain. New snow amounts taper with elevation and lie over a supportive crust at about 1300 metres and below. At higher elevations, the recent snow is incrementally loading a weak interface that was buried in late February. The interface is composed of facets, crusts, and surface hoar and may be 40-60 cm deep. There's uncertainty about the distribution and reactivity of this interface, but it recently proved reactive under skier traffic in the north of the region. The mid-pack is well consolidated, but sits above weak, sugary snow near the ground. This deeper basal weakness remains an ongoing concern in thin rocky start zones and in shallow snowpack locations.

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