Bulletin d’avalanche

South Coast

Apr 18 – 19, 2016Avalanche Canada
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Archivé · expiré 10 years ago

Danger d’avalanche

Wed
Thu
Alpin
Sans niveau
Limite forestière
Sans niveau
Sous la limite
Sans niveau
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Points saillants

Spring Conditions. Sunny skies and very high freezing levels will increase the avalanche danger. The surface crust holds the snowpack together and may break down rapidly if there is no re-freeze overnight.

Problèmes avalancheux

  • Cornices

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible - Likely
    Taille
    2–5
    Strong solar radiation and high freezing levels will continue to test remaining cornices in the alpine. Watch your overhead hazard and avoid traveling beneath corniced ridges.

  • Loose Wet

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely
    Taille
    1–3
    Sunny skies and high freezing levels will weaken the surface snow on solar aspects. Shaded aspects in the alpine may warm up enough to release as loose wet avalanches.

  • Wet Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely - Possible
    Taille
    2–6
    The likelihood of wet slab avalanches will increase over the next few days with forecast high freezing levels and strong solar radiation. Be especially careful at mid and lower elevations where the entire snowpack is sloppy and unsupportive.

Weather Forecast

Overnight freezing level at 3500 metres under clear skies with light southwest winds. Clear and sunny on Tuesday with light southwest winds and freezing levels at 3500 metres. Clear and sunny on Wednesday with light winds and freezing level at 3500 metres. Some uncertainty regarding when the ridge of high pressure will break down; at this time about 50-50 chance of sun or cloud on Thursday. Freezing levels will start to drop after the ridge breaks down and moves eastward.

Avalanche Summary

No new avalanches reported, but we have very few eyes and ears still in the mountains reporting. Most commercial operations in the region have finished their season and data is sparse.

Snowpack Summary

Cornices are large, fragile, and could trigger deep slab avalanches that run to valley bottoms. Monitoring the overnight freeze of the snow surface is very important.. If the snow surface does not freeze overnight or if the crust is only a few cm thick, the effect of daytime heating and solar radiation will weaken the snowpack much quicker. There is an old crust layer down approximately 50cm in the Duffey area and north of Pemberton. Though mostly dormant, it produced a couple large avalanches during the last major warming event. The forecast hottest weather of the year to date could again test it, especially in isolated locations such as steep, rocky faces. Glide cracks are widespread, active, and best avoided. Low elevation and thin snowpack areas have become isothermal, meaning the snowpack is 0 degrees Celsius throughout. An isothermal snowpack is more prone to full depth wet slab avalanches during the heat of the day, especially on steep, smooth slopes.

Régions couvertes