Bulletin d’avalanche

Purcells

Feb 6 – 7, 2015Avalanche Canada
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Archivé · expiré 12 years ago

Danger d’avalanche

Sun
Mon
Alpin
4 · Fort
Limite forestière
4 · Fort
Sous la limite
3 · Marqué

Points saillants

The warm, wet, and windy storm continues to result in HIGH avalanche danger.

Problèmes avalancheux

  • Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible - Likely
    Taille
    2–5
    Buried persistent weak layers may be over-loaded by the forecast new storm snow resulting in human triggering, or storm slab avalanches in motion stepping down to the deeply buried weak layers.
  • Storm Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely
    Taille
    2–5
    Strong winds, heavy snowfall, and high freezing levels are expected to continue the widespread natural avalanche cycle.
  • Deep Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Unlikely - Possible
    Taille
    3–6
    Deeply buried weak layers may react to large loads like an avalanche in motion. Rain soaked areas may release as wet slab avalanches and run to valley bottoms.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Strong Southwest winds and heavy precipitation are expected overnight combined with the freezing level staying at about 1600 metres in the North and about 2100 metres in the South. Light to moderate precipitation and moderate Southwest winds during the day on Saturday. Light precipitation and light Southerly winds on Sunday with freezing levels starting to drop slowly. Another pulse of moderate precipitation with light winds on Monday.

Avalanche Summary

Natural and explosive controlled avalanches up to size 2.5 reported releasing in the storm snow. I suspect that there was a widespread natural avalanche cycle on Friday. Limited reports due to poor visibility and limited travel.

Snowpack Summary

The new storm snow is now 25-40 cm thick and has been heavily wind affected, developing thick areas of wind transported snow that may be easy to trigger. The new storm slab sits on a variety of old surfaces, including hard crusts, breakable crusts at higher elevations, and surface hoar in some areas. A melt freeze crust can be found up to about 2200m. At higher elevations, the surface is heavily wind affected. The depth of the mid-January surface hoar is highly variable across the region and it may have been destroyed by warmth at low elevations. Where it does exist, it can be found between 30 and 70 cm below the surface. The mid-December surface hoar layer lies below a strong mid-pack down about 60 to 120cm. Both of these persistent layers have been reactive recently. The mid-November weak layer of crusts and facets can still be found near the bottom of the snowpack. It has been unreactive lately, but should be on your radar in shallow snowpack areas where there is more chance of triggering.

Régions couvertes