Boletín de aludes

Lizard-Flathead

Dec 25, 2017Avalanche Canada
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Archivado · caducó 9 years ago

Peligro de aludes

Tue
Wed
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

Dress warm if you go out for a Christmas ride and watch for areas where the snow feels stiff or slabby.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Expect slabs at higher elevations where northerly winds have formed hard deposits of snow on the downwind sides of ridges and gullies.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    A layer of surface hoar buried 50-70 cm below the surface has the potential to produce surprising avalanches. Triggering this layer is most likely in on steep sheltered slopes at treeline and below.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

MONDAY: Clouds clearing throughout the day, light north winds, treeline temperatures around -20 C.TUESDAY: Mix of sun and cloud, moderate west winds, treeline temperatures around -20 C.WEDNESDAY: Mix of sun and cloud, moderate west winds, treeline temperatures around -17 C.

Avalanche Summary

Avalanche activity has quieted down as the cold weather sets in, although there have been some isolated reports of whumpfs at small avalanches failing on the mid-December surface hoar layer at lower elevations (e.g. see this Mountain Information Network report). Also, read the current forecasters' blog for more advice on managing the current conditions (click here).

Snowpack Summary

Cold temperatures are preserving 50 to 70 cm of fresh snow from the past week. The snow has been deposited into harder wind slabs in exposed terrain, but remains low density in sheltered areas. The main question in the snowpack surrounds the mid-December layer sitting beneath the new snow. The layer includes crusts on south and west facing slopes and large feathery surface hoar crystals in sheltered terrain at and below treeline. The distribution of the layer, as well as the properties of the snow above it, is variable. The most suspect areas are where the wind has formed a stiff slab above this layer and on slopes with preserved surface hoar. The lower snowpack is generally well settled with a thick prominent crust that was buried near the end of November.

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