Bollettino valanghe

Purcells

Dec 14 – 15, 2013Avalanche Canada
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Archiviato · scaduto 13 years ago

Pericolo valanghe

Mon
Tue
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

Additional snow, wind, and warm temperatures will determine the hazard in the next few days.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–3
    Be cautious of terrain that has been recently wind-loaded
  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–5

Confidence

Fair - Timing of incoming weather systems is uncertain

Weather Forecast

Sunday: Moderate snowfall with 10-15cm of accumulation, freezing levels rising up to 1800m and strong southwesterly winds. Forecast models show a bit more precipitation in the south. Freezing levels expected to remain at or near valley bottoms with tree line temperatures around -8. Ridge top winds are expected to be moderate westerlies. Monday: Little snowfall expected with less than 5cm of accumulation at higher elevations, freezing levels will rise to around 1500m with strong westerly winds. Tuesday: Moderate to locally heavy snowfall as a Pacific frontal system moves into the interior. Strong westerly winds and freezing levels rising to 1800 metres in parts of the forecast area.

Avalanche Summary

Avalanche activity has been limited to a few loose sloughs from steep terrain. On Tuesday, a wind slab avalanche size 1.5 was easily triggered under the weight of a rider on a NE aspect. Also a large ( 2.5) natural avalanche was reported in the interior of the Purcells on an E aspect. The potential exists for large destructive avalanches with increased loading.

Snowpack Summary

Recent snow and winds are adding to the surface load. Snowpack depths at tree line currently vary from 70 - 110 cm with the highest variability in wind-exposed areas. A persistent weakness of buried surface hoar and facets, along with an associated crust, is down approximately 20-40cm . This layer has been producing variable results with snowpack tests, and may become reactive as a cohesive slab develops with warming temperatures and additional loads. At the base of the snowpack are weak facets and depth hoar. This deep persistent weakness may be stubborn to trigger, especially in deeper snowpack areas, but the sensitivity to triggers likely increases in shallower locations, especially on steep, convex slopes.  At lower elevations the snow depth is below the threshold for avalanches.

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