Boletín de aludes

Purcells

Jan 18 – 19, 2012Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Fri
Sat
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

Conditions in the alpine are variable across the region. Areas with minimal wind loading are MODERATE.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–3
    Wind slabs have formed recently, causing large avalanches in some areas. Be alert for wind slabs behind ridges and ribs, especially on east and north-facing slopes.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    4–7
    Two layers to watch: 1. Buried surface hoar, most likely triggered on steep, unsupported slopes amongst the trees. 2. Basal facets, triggerable from thin snowpack areas or by a very heavy load (cornice fall, airborne sled). Avalanches could be large.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    3–6
    Susceptible to human triggers particularly from thin spots on slopes with variable snow distribution, heavy impacts, or deep penetration. If triggered, slabs are likely to release across wide areas.

Confidence

Good - -1

Weather Forecast

Thursday: One more day of frigid cold to endure - although some minor warming may creep into the far south. Light winds. No precipitation.Friday: Light snow starting late in the day. Moderate south-westerly winds and temperatures rising slightly. Saturday: Continued light to moderate snowfall. South-westerly winds.

Avalanche Summary

A natural avalanche cycle to size 2.5 was reported on alpine slopes in the northern Purcells, failing in response to an overnight wind event. Skiers have been triggering soft slabs in steep terrain in the size 1-1 .5 range over the past few days, however many observers say that the snow remains mostly cohesionless due to the intense cold.

Snowpack Summary

20-45 cm of low density storm snow has been redistributed by mainly south-westerly winds. Cold temperatures have limited the widespread development of storm slabs, but wind slabs and cornices of variable reactivity have built up. Below the storm snow are various surfaces including facets, surface hoar in sheltered areas, wind crust, soft slabs and hard slabs. The mid-December surface hoar/facet persistent weakness, now down around 50cm on the eastern side of the range and as deep as 160cm on the western side, is still causing operators concern, especially in shallow snowpack areas. The consequences of a failure on this layer would be large. Facets and depth hoar exist at the base of the snowpack.

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