Boletín de aludes

South Columbia

Apr 13 – 14, 2013Avalanche Canada
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Archivado · caducó 13 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

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–6
    A layer of surface hoar is buried about a metre down, mainly on high northerly aspects. A surface avalanche stepping down, cornice fall, or the weight of a person from a thin-spot trigger point could trigger it.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    Snowfall on Friday night and variable winds have created new storm slabs, especially near ridge top and on slopes in the lee of the wind.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Sunday: Very light snowfall / Light northeast winds / Freezing level at 1400mMonday: Mix of sun and clouds / Light east winds / Freezing level at 1400mTuesday: Mix of sun and cloud / Calm winds / Freezing level at 1600m

Avalanche Summary

Observations are becoming more limited; however a size 2 natural wind slab avalanche was observed on a lee alpine feature on Friday. A size 2 slab was also ski cut on a steep southeast facing convex roll. Surface hoar was the suspected interface.I would expect ongoing storm instabilities in the wake of new snow and wind on Friday night.

Snowpack Summary

Moderate to locally heavy snowfall on Friday night has created touchy new storm/wind slabs, especially near ridge top. This will add to existing storm slab and wind slab problems at alpine and treeline elevations. A surface hoar interface is buried within the upper metre or so of the snowpack, mainly on high-elevation northerly aspects. It may be slowly gaining some strength, but these slopes should still be treated with suspicion. On other slopes, recent storm snow overlies a crust, with a variable bond. At low elevations, moderate accumulations overlie previously rain-soaked snow which is now refrozen and strong.Recent wind and snow has added to the size and fragility of large cornices.

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