Bulletin d’avalanche

Northwest Coastal

Dec 28 – 29, 2011Avalanche Canada
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Archivé · expiré 15 years ago

Danger d’avalanche

Fri
Sat
Alpin
4 · Fort
Limite forestière
4 · Fort
Sous la limite
3 · Marqué

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Very Likely - Certain
    Taille
    2–7
    Deep wind slabs are likely in exposed lee and cross-loaded terrain in the alpine and at treeline.
  • Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely
    Taille
    1–6
    There is a possibility of highly destructive avalanches where the deeply buried mid-December crust/facet layer persists.
  • Storm Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Very Likely
    Taille
    1–6
    Storm slabs are growing in size and likelihood and may be triggered naturally or by the weight of a person.

Avalanche Summary

Highways avalanche control produced numerous Size 2-3.5 slab avalanches on Tuesday. I suspect there was a fairly widespread avalanche cycle in backcountry areas on Monday and/or Tuesday, and this cycle may continue for another day or two as another system is forecast to bring moderate to heavy snow and strong winds again tonight.

Confidence

Poor - Timing of incoming weather is uncertain

Weather Forecast

Wednesday night and Thursday: Another system arrives bringing 20-30cm of snow, tapering off on Thursday afternoon. The freezing level drops from 1000m to valley bottom overnight. Winds are strong from the SW. Friday and Saturday: Mainly cloudy with light snowfall (maybe 5-10cm each day). Freezing level at valley bottom. Winds are light to moderate from the SW.

Snowpack Summary

Over the past week the northwest has been slammed by snow, strong to extreme winds, and fluctuating freezing levels. The weeks tally is closing in on 200cm near Terrace, with areas to the north seeing a little less (Stewart up to 120cms). Alpine observations have been limited and wind sensors have been disabled by rime, but I suspect new snow has been blown around by strong southwest winds creating wind slabs on lee slopes and scoured windward slopes.In addition to the more obvious direct-action storm instabilities that are expected with the forecast weather, local avalanche professionals have some other concerns: Surface hoar that formed during the winter solstice sits approximately 40-60cm below the surface and may become more reactive with more wind and snow. As well, the crust-facet combo (extends up to alpine elevations in the south and to 1000m in the north) from the early december dry-spell sits about 150cm below the surface and has not gone away. Any avalanches on this layer would be highly destructive and are probably waiting for the right load or trigger.

Régions couvertes