Bollettino valanghe

Purcells

Feb 24 – 25, 2015Avalanche Canada
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Archiviato · scaduto 12 years ago

Pericolo valanghe

Thu
Fri
Alta quota
2 · Moderato
Limite del bosco
1 · Debole
Sotto il limite
1 · Debole

In sintesi

If warming persists, there will be a higher likelihood of avalanche activity, especially on steep, sun-exposed slopes.Are you a member of Avalanche Canada? Join today at avalanche.ca/membership

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    3–5
    Destructive persistent slab avalanches have become less likely to trigger. Possible triggers include solar radiation or a large cornice fall. I'd limit my exposure to big overhead terrain, especially if the sun is shining and temperatures are warm.

Confidence

Fair - Due to the number of field observations

Weather Forecast

The current ridge of high pressure will persist through Wednesday bringing a mix of sun and cloud. On Thursday and Friday, however, a weak disturbance will track across the region, although only light amounts of snow and overcast skies are expected. Freezing levels should hover around 800m for the period with ridge top winds remaining generally light from the northwest.

Avalanche Summary

Under Monday's warm skies, loose wet avalanches to size 2 were observed in sun-exposed terrain. That said, observations were limited, and the warming may have had a more widespread effect. In the neighboring North Columbia region, warming and solar radiation triggered some persistent slab avalanches to size 3.5. Forecast cooling should limit avalanche activity of this nature.

Snowpack Summary

Generally light amounts of loose cold snow cover the previous variable snow surface of crusts, surface hoar, dry facetted snow, or wind affected snow depending on aspect and elevation. Thin wind slabs may still be sensitive to triggering in isolated high elevation lee terrain, and cornices remain large and weak. The 'Valentine's Day' crust, found just below the surface, is thick and supportive below 2100 m. The late-Jan crust/surface hoar layer is 1-2 m deep in the west, and can be found within the upper metre of the snowpack further east. It is variably reactive in snowpack tests and still the main concern in many areas. The mid-January surface hoar, deeper again, is also a concern in some areas. Deeper weakness are likely to remain dormant for the time being.

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