Boletín de aludes

South Columbia

Apr 19 – 20, 2015Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

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

Danger ratings reflect conditions during the hottest parts of the day. Time your travel to take advantage of cool temperatures. Danger ratings end today, but check back for spring and summer advice.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–5
    Large cornices are expected to become weak with daytime warming, especially when exposed to the sun. Cornices have the potential to trigger large slab avalanches.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    A touchy interface down 40-60 cm may be triggered by people or with a natural trigger like cornice fall or sunshine.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1–4
    Strong sunshine is expected to trigger loose wet avalanches on steep sun-exposed slopes. These have the potential to trigger larger slab avalanches.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Monday should bring warm, dry weather with light winds. The freezing level climbs to 2600 m.

Avalanche Summary

A round of solar-triggered loose wet and wet slab avalanches was observed on Friday and Saturday. A size 2 slab also failed naturally on a NE aspect at ridge top. Whumpfing continues to be reported in the Selkirks.On Thursday, skiers remotely triggered size 1-2 slabs (from 40 m away) on SE-NE aspects between 2000 and 2450 m. These all failed on the April weak layer, around 40 cm down. There was also a natural loose and slab avalanche cycle on solar aspects up to size 2.5.Avalanche activity is expected to continue as the temperatures rise.

Snowpack Summary

A troublesome weak layer is down 40-60cm. This layer consists of surface hoar and facets overlying a melt-freeze crust. In exposed alpine terrain, recent strong SW winds formed wind slabs in leeward features. Large cornices exist and may become weak with daytime warming. There are three dormant persistent weak layers that we are continuing to track. The late-March crust is down 50-70cm and was reactive last week during the warm period. The mid-March and mid-February layers are typically down between 70 and 100cm and have been dormant for several weeks. These layers have the potential to wake up with sustained warming, a significant rain event, and/or a big cornice fall.

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