Boletín de aludes

Sea To Sky

Apr 11 – 12, 2012Avalanche Canada
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Archivado · caducó 14 years ago

Peligro de aludes

Fri
Sat
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil
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Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Wind slabs exist below ridges in some areas. These could be triggered by the weight of a person.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–7
    Persistent slab avalanches have become less likely, but remain possible, especially with a large trigger like cornice fall.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–4
    Warm temperatures may continue to weaken surface snow, especially at low elevations. Avoid traveling above terrain traps or under any slopes which have glide cracks.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain

Weather Forecast

Thursday: A mix and of cloud, sun and light precipitation. Freezing level around 1600 m. Light southerly winds.Friday: Light precipitation, dissipating. Light winds. Freezing level around 1500 m. Saturday: Clearing skies. Light south-westerly winds. Freezing level rising to around 2000 m.

Avalanche Summary

On Tuesday, several size 1-2 loose moist avalanches were triggered by solar warming or by people. On Sunday, a natural and human-triggered wind slab cycle occurred on north-west and west aspects following overnight winds. A size 3 natural slab is suspected to have stepped down to the March crust on Monday. It failed on a sun-exposed south-west aspect at 2300 m. There has also been some cornice fall.

Snowpack Summary

A melt-freeze crust exists on solar aspects and at low elevations. In some areas, limited overnight cooling has kept surface snow from re-freezing, leaving it loose and cohesionless. Areas of wind slab formed with recent southerly or easterly winds. Pockets of snow can be found on high north aspects, now buried underneath wind slabs in some areas. A predominately crusty weak interface from late March, now down 50-190 cm, has become less likely to trigger, but remains a lingering concern.

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