Boletín de aludes

Northwest Inland

Mar 22 – 23, 2015Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Tue
Wed
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil

Lo esencial

Watch for new wind slabs forming with light snowfall forecast for Monday.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Small wind slabs may form in response to new snow and wind on Monday morning. Watch for triggering in gullies and in the lee of ridge crests in upper elevation terrain.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Monday

Weather Forecast

Scattered snowfall (up to 5cm) is expected on Monday as a cold front moves over the region. Due to the convective nature of the snowfall, more intense precipitation may result in some areas. By late Tuesday, a ridge should bring clearing that should last until late Wednesday. By Wednesday evening, a more organized warm and wet frontal system will arrive. Ridgetop winds should be moderate from the southwest with Monday's snowfall, decreasing to light on Tuesday. Freezing levels should hover around 1200m on Monday and Tuesday, rising to about 1800m with Wednesday's system.

Avalanche Summary

Numerous size 1 loose wet avalanches were reported on Saturday. They failed in steep rocky terrain in response to warming and solar radiation. Cloud on Monday should limit this type of pattern, although there may be a shift to small wind slab activity with light convective snowfall forecast for Monday morning.

Snowpack Summary

Light accumulations from Friday may now exist as a soft wind slab in high elevation lee terrain. The new snow overlies older wind slabs, crusts and wind-scoured surfaces. Sun-exposed slopes and lower elevation areas are likely in a spring melt-freeze cycle. Weaknesses buried in the upper snowpack may include hard crusts and/or facet crystals, although not much is known about the reactivity or spatial distribution of this layer. At the base of the snowpack, weak facets may be found. Cornices are large and potentially fragile, especially under warm, sunny skies

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