Boletín de aludes

Northwest Inland

Apr 6 – 7, 2016Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

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

Extreme warming and solar radiation will drive the Avalanche Danger. Be alert to conditions that change throughout the day, and watch your overhead hazard. Very large avalanches may reach their run-out zones.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–5
    Some cornices are the size of a bus. As temperatures rise and sunny weather makes a come-back, these monsters will become more likely to fail. A large cornice fall may be the trigger required to initiate destructive persistent slab avalanches.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    In high elevation lee terrain hard storm slabs may remain reactive to light loads with the potential for wide propagations. In areas more affected by heat and sun, the new snow may react as a wet slab.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    1–4
    Rising freezing levels on Thursday will promote loose wet avalanche activity, especially in steep sun-exposed terrain. Loose wet avalanches can entrain mass quickly and run long distances. Be alert to conditions that change throughout the day.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

A dry ridge of high pressure will bring mainly clear skies for Thursday and Friday. Increased cloud and isolated flurries are forecast for Friday evening and Saturday. The freezing level will spike to about 2800m on Thursday and then hover around 2400m on Friday and Saturday. Ridgetop winds will remain mainly light and variable.

Avalanche Summary

Stormy weather has limited avalanche observations, although I'm sure there was a decent round of natural storm slab activity in response to new snow and wind on Tuesday. As the sun comes out and temperatures rise, cornice failures, loose wet, wet slab and isolated deep persistent slab avalanches should be on your radar.

Snowpack Summary

On Tuesday, 10-20cm of new snow fell. Throughout the storm, extreme westerly winds promoted continued cornice growth and created a widespread wind effect at higher elevations. About 30cm below the surface you'll find a widespread hard melt-freeze crust that formed as a result of last week's warm weather and more recent cooling. A few persistent weak layers exist in the snowpack including lingering surface hoar layer from January (down over a meter), and weak basal facets at the bottom of the snowpack. The near-surface crust has dramatically limited the reactivity of these destructive old layers; however, they have the potential for isolated yet very large avalanches with forecast warming and solar radiation.

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