Boletín de aludes

Kananaskis

Apr 27 – 28, 2014Alberta Parks
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Archivado · caducó 12 years ago

Peligro de aludes

Tue
Wed
Alta montaña
1 · Débil
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil
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Lo esencial

Still some good skiing found on sheltered North aspects at higher elevations. However, watch for rapid rises in avalanche danger related to solar radiation and warm temperatures. Start early and finish early.

Problemas de aludes

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Timing is everything at this time of year. Solar radiation is intense and can lead to rapid destabilization of the snowpack. Air temperatures are also a concern as the snowpack grows isothermal at lower elevations later in the day.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    3–6
    The basal facets are producing large slab avalanches that are failing on the basal facets.

Confidence

Good

Weather Forecast

Wednesday should be mostly sunny with NW winds gusting to 55 km/h. Alpine temperatures should reach -3 degrees with freezing levels near 1700m. The rest of the week will see a warming in temperatures with freezing levels near 3100m by Thursday.

Avalanche Summary

Nothing new observed today, but a size 3.0 slab avalanche occurred on Commonwealth Ridge sometime Saturday. This was a full-depth avalanche on a SE aspect that ran full path and destroyed mature timber.

Snowpack Summary

Between 2 and 8cm of new snow overnight depending on aspect and elevation. This overlies a melt freeze crust on all aspects at all elevations except for North aspects above 2400m. Isolated thin wind slabs are found at ridge-crest in immediate lee slopes, but generally don't seem to be reactive to ski cutting. The basal facet and depth hoar remain a concern during times of intense heating and/or solar radiation. Where cornices exist they are large and sagging.

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