Bollettino valanghe

South Rockies

Dec 5 – 6, 2015Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 11 years ago

Pericolo valanghe

Mon
Tue
Alta quota
Senza grado
Limite del bosco
Senza grado
Sotto il limite
Senza grado
Apri la mappa completa

In sintesi

Strong SW winds are likely forming stiff wind slabs at upper elevations. The snowpack is highly variable. Give info and get info! Check out the Mountain Information Network. (MIN)

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–3
    You're likely to find small storm slabs in wind sheltered terrain. Wind exposed terrain is a different story. Where the wind is blowing, I expect a growing wind slab problem that will likely increase in sensitivity to triggering throughout the day.

Confidence

Low - Due to the number of field observations

Weather Forecast

Strong southwesterly flow is expected to continue to drive moist and progressively warmer systems into the Coastal and Interior ranges of the province, but very little is expected to spillover into the southeast corner. SUNDAY: Freezing level 1800m. No significant snowfall expected. Strong SW winds at all elevations. MONDAY: Freezing level beginning around 1800m rising to 2000m. 1 to 10cm of snow possible. Strong SW winds at all elevations. TUESDAY: Freezing level could peak as high as 2500m. Trace of snow/rain possible. Strong to Extreme SW winds.

Avalanche Summary

No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.

Snowpack Summary

15 to 25cm of recent low density storm snow sits on the surface, or has been sluffing from steeper terrain features. The new snow sits on a variety of older snow surfaces which consist of stubborn wind slabs and crusts in exposed higher elevation terrain, and loose faceted snow and surface hoar in more sheltered areas. Above treeline 100-150 cm of snow sits on the ground, while below treeline you may only find 40-90 cm. Several rain crust layers exist within the snowpack, one down approximately 30-60 cm (mid-November) and another down 10-25 cm depending on elevation. Snowpack test results have shown easy shears, failing in a facet layer below the crust. Definitely something to keep an eye on when we receive more load. Where this crust exists, it has added strength to the current snowpack. In general there is a lot of uncertainty regarding snowpack structure throughout the region

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