Boletín de aludes

South Columbia

Nov 28 – 29, 2015Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

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

Warming temperatures may push the danger ratings higher, especially on solar aspects. A big THANK YOU ! to all those posting on the MIN

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3
    Northerly winds have formed wind slabs on south aspects where we don't usually see them.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    The warm temperatures at upper elevations may significantly warm the snowpack on solar aspects and create a loose wet hazard, Use caution on sun-drenched slopes at this time.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely
    Tamaño
    2–5
    Weak-facetted snow at the base of the snowpack may exist on north aspects in shallow areas. An avalanche on this layer could be large and destructive.

Avalanche Summary

Some snowballing from warm temperatures on steep solar aspects, and small loose, dry snow sluffing on steep north facing slopes

Confidence

Fair - Due to the number and quality of field observations

Weather Forecast

An arctic high continues to dominate the weather pattern over western Canada. Blue skies and dry conditions are not forecast to move out of the area until Tuesday or Wednesday next week. In the meantime, an above-freezing layer (AFL) of air will pass through the region between 1500 and 3000m bringing temperatures in that elevation band to as high as +5c., and possibly higher on solar aspects. Arctic air pooling in the valley bottoms will keep the temperatures well below freezing until the next storm system flushes out the cold air.

Snowpack Summary

The snowpack is extremely variable at this time, with wind scoured North facing slopes at treeline and above. South facing slopes have wind slabs at tree line and above, and may be hiding surface hoar from the previous spell of cold clear weather. Surface facetting has been observed in the region as a result of the recent cold weather and clear skies, and there will be surface hoar building in sheltered locations. There are a number of surface hoar layers now buried in the snowpack that at present seem to be unreactive, with the most recent having been buried on Nov 24th.In shallow snowpack areas, especially on northern aspects, there may be a weak facetted layer at the base of the snowpack.

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