Bollettino valanghe

Kootenay Boundary

Jan 8 – 9, 2015Avalanche Canada
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Archiviato · scaduto 12 years ago

Pericolo valanghe

Sat
Sun
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
2 · Moderato

In sintesi

It's important to make conservative terrain choices even though the avalanche danger is slowly decreasing. The consequences of triggering a persistent slab remain high.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–5
    There is potential to trigger avalanches on a weak layer buried 80-100 cm deep. Be vary wary of slopes that did not slide slide during the last storm and be aware of the potential for triggering slabs from a distance.
  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–4
    Forecast sunshine and mild temperatures could maintain touchy storm slab conditions and trigger loose wet slides on steep sun-exposed slopes.

Confidence

Fair - The weather pattern is stable

Weather Forecast

Synopsis: A strong ridge of high pressure should maintain dry conditions with possible valley cloud for at least the next few days. A slight temperature inversion should stick around through Saturday with mountaintop temperatures getting close to 0 degrees. A weak upper trough slides across the province on the weekend, but this might only result in a bit more mid-level cloud and a chance of flurries. By Sunday the inversion should disappear. Winds are light gusting to moderate from the W-NW throughout the period.

Avalanche Summary

Most areas reported a fairly widespread and large natural avalanche cycle on Tuesday. Many of these slides stepped down to mid-December persistent weak layer and produced avalanches up to Size 3.5. There were also reports of skiers and machines triggering slab avalanches from a distance (remotely and sympathetically triggered). Most reported avalanches occurred above 1900-2000 m from a variety of aspects.

Snowpack Summary

Warm temperatures and previous rain have probably created a surface crust on steep solar aspects and all slopes below around 1800 m. Dry powder can still be found at higher elevations. Around 30-60 cm of settling storm snow overlies a variety of old surfaces which include heavily wind-affected surfaces in exposed locations, faceted powder and buried surface hoar in sheltered terrain. Buried 80-100 cm deep, you'll likely find a touchy weak layer of surface hoar sitting on a thick rain crust. This widespread persistent weakness exists at all elevation bands, and continues to be the primary layer of concern for the region. With the recent load of storm snow, I expect this layer to remain active with the potential for large and destructive avalanches. At the base of the snowpack, a crust/facet combo appears to have gone dormant for the time being.

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