Boletín de aludes

Purcells

Jan 26 – 27, 2016Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Thu
Fri
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
2 · Moderado

Lo esencial

Strong winds and rising freezing levels are pushing the danger ratings up. Conservative terrain choices without overhead hazards are recommended at this time.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–3
    New wind slabs continue to develop with forecast new snow and wind. Rising freezing levels may increase the likelihood of triggering these touchy wind slabs.
  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–5
    Rising freezing levels and increased loading from wind, snow, and rain, may increase the likelihood of triggering the buried weak layer of surface hoar.

Confidence

Moderate

Weather Forecast

Clouds and light snow overnight combined with increasing westerly winds. Freezing levels rising on Wednesday up to about 2000 metres with moderate westerly winds in the alpine. Snow starting early Thursday morning, expecting 5-10 cm during the day above 1500 metres, with rain below treeline. Gradual cooling with light wind and light snow on Friday.

Avalanche Summary

No new natural avalanches reported from Monday, however explosives control produced slab avalanches up to size 3.0.  A couple of natural avalanches were reported on Sunday but most of the natural avalanches occurred on Friday and Saturday due to storm loading. While natural activity has tapered off since Saturday, the persistent slab is expected to remain reactive to human triggering for several more days. New wind slabs are developing in the alpine and at treeline.

Snowpack Summary

Conditions are widely variable across the Purcells. Wind slabs and storm slabs have developed at treeline and alpine elevations. In some areas, these overlie a surface hoar or crust/facet interface from early January and may be easily triggered by a skier or sledder. Reports indicate this persistent weak layer is now typically down 40 to 60cm in most areas and appears to be quite touchy in some parts of the region. A more deeply buried layer of surface hoar from December is now considered dormant. In general, the lower snowpack is well settled and strong.

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