Boletín de aludes

Purcells

Mar 19 – 20, 2019Avalanche Canada
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Archivado · caducó 8 years ago

Peligro de aludes

Thu
Fri
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
4 · Fuerte

Lo esencial

The hot and sunny weather persists on Wednesday, which will likely continue the natural avalanche cycle. The danger will be the highest when the day heats up, so make sure you are completely out of avalanche terrain, with no overhead exposure.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1.5–3
    A cohesive slab of snow is poorly bonded to weak, sugary faceted snow or a melt-freeze crust. The warm temperature and strong sun has increased the likelihood of triggering a slab avalanche by humans, cornices, and naturally.
  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    1–3
    The upper snowpack has destabilized with warm air temperature and strong sunshine, which has produced large avalanches (to size 3). The most problematic time is with maximum warming during afternoon hours.

Confidence

High -

Weather Forecast

TUESDAY NIGHT: Clear skies, light south wind, alpine temperature 5 C, freezing level 3200 m.WEDNESDAY: Clear skies, light southeast wind, alpine temperature 6 C, freezing level 3400 m.THURSDAY: Clear skies, light southeast wind, alpine temperature 5 C, freezing level 3100 m.FRIDAY: Clear skies, light southeast wind, alpine temperature 4 C, freezing level 2900 m.

Avalanche Summary

Many wet loose avalanches were observed on Tuesday, from small to large (size 1 to 3). They occurred on southeast to southwest aspects and at all elevations. A wet slab avalanche was also observed on a south aspect with a depth of 60 cm, likely releasing on the weak layer described in the snowpack summary.This avalanche cycle is expected to continue, as temperatures remain exceptionally warm and the sun shines strong.

Snowpack Summary

A cohesive slab of snow around 20 to 30 cm thick overlies weak and sugary faceted snow or a melt-freeze crust on sun-exposed slopes. Natural avalanches are expected to continue at this interface.Below treeline, a weak layer of faceted grains and/or feathery surface hoar crystals buried in mid-January can be found around 50 to 90 cm deep, which may be combined with a melt-freeze crust on south aspects. The current warm conditions may awaken this layer, resulting in large, destructive avalanches. Steep cutblocks and large open glades at lower elevations are the most likely places to trigger this layer. Smaller loose wet avalanches may trigger this layer.The base of the snowpack is composed of weak faceted snow, which may be associated with a melt-freeze crust. The warm air and sunny skies could increase the likelihood of triggering very large avalanches on this layer.

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