Bollettino valanghe

Northwest Inland

Dec 25 – 26, 2013Avalanche Canada
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Archiviato · scaduto 13 years ago

Pericolo valanghe

Fri
Sat
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato
Apri la mappa completa

In sintesi

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–5
    A couple of week layers from earlier in the month are lurking in the top meter of the snow pack. Continued loading and settlement of the overlying snow may increase the likelihood of triggering an avalanche one of these layer.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    Recent snow combined with suspected strong winds are likely loading lee features. Watch for wind slabs.

Confidence

Poor - Wind speed and direction is uncertain

Weather Forecast

Synopsis: The next frontal wave with push onto the north coast early Thursday morning causing temperatures to spike before it shifting southwards. Expect light precip Thursday followed by a clearing trend into the weekend.Tonight and Thursday. Snow amounts: 10 to 15 cm falling as rain at lower elevation. Freezing levels: Rising to 1500m. Ridge winds: Moderate south-westerly. Friday. Snow amounts: light flurries. Ridge winds: Moderate south-westerly. Alpine temps: -5Saturday. Snow amounts: nil , Ridge winds Light westerly. Alpine temps: -5.

Avalanche Summary

No new avalanche have been reported.

Snowpack Summary

There is significant variation in snow depths across the region. In the Smithers area the ski hill is reporting an 111 cm base with the Ashman trailer is around the same. Treeline depths vary between 100 - 200 cm.The region has received up to 10cm of snow in the last 24 hours. Between 30 and 80cm of snow now rests upon a crust that extend up to treeline and possibly beyond. This interface has been popping under easy loads in snowpack tests.We don't have great wind stations in the region, but the coast saw a lot of strong wind during the last storm & I suspect this region was similarly hammered, forming windslabs in the alpine and at treeline.Deeper in the snow pack a layer of facets/surface hoar formed during the early December cold/dry spell can be found in the top 100cm in the Ashman . The mid and lower snowpack is still structurally weak and faceted. Depth hoar and an early season crust exist near the ground.

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