Boletín de aludes

Northwest Inland

Mar 30 – 31, 2017Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

Sat
Sun
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

Forecast new snow and wind are expected to develop new wind slabs in the lee of southwest winds.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2
    Expect new wind slabs to develop due to the forecast new snow and wind.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely
    Tamaño
    1–3
    A weak layer of facets and/or a crust that developed early in the winter lies near the bottom of the snowpack. Any change in the weather may affect the likelihood of triggering this deep weak layer.

Avalanche Summary

Storm slabs up to size 2.5 were reported from the western extent of the region in the Howson's, where the snowpack is more like the Northwest Coastal region. No new avalanches reported from the rest of the region.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Friday

Weather Forecast

Overnight: Cloud and strong southwest winds developing overnight, with 3-5 cm above 700 metres by morning. Friday: Overcast with strong southwest winds, another 3-5 cm during the day with daytime freezing up to 1200 metres. Saturday: Overcast with a few cm of new snow and moderate southwest winds. Sunday: Overnight freezing down to valley bottoms. Overcast with flurries or light snow and moderate westerly winds.

Snowpack Summary

Light snow combined with moderate southwest winds has developed wind slabs in the alpine and in some exposed treeline locations. Periods of sun and high daytime freezing levels have developed crusts below treeline and on sun exposed terrain at all elevations. The snow may be moist or wet below treeline during the warmest part of the day. The Mid-February crust and facet layer was reported to be down 75-90 cm in the Houston Telkwas sled area on Wednesday. The deep persistent weak layer of facets and/or a crust that were buried early in the winter are still lingering near the bottom of the snowpack. This MIN report found the deep weak layer strengthening in the Telkwas.

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