Bollettino valanghe

Cariboos

Apr 4 – 5, 2012Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 14 years ago

Pericolo valanghe

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

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–5
    Generally lurking below ridgecrests, behind terrain features, and in gullies. Thick fresh wind slabs are highly sensitive to human triggers and cornice falls, and sun-exposure is expected to make things even more touchy.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–4
    Large and weak cornices could easily start popping off with sun-exposure. Not only are they a hazard in themselves, but can also act as a heavy trigger for very large avalanches on the slope below.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    Steep rocky terrain in the afternoon. Wet loose avalanches can entrain significant mass and run long distances.

Confidence

Good

Weather Forecast

Thursday and Friday: unsettled conditions with isolated light flurries interspersed with intense sunshine. Freezing levels hovering around 1000m-1200m and light to moderate northerly ridgetop winds. Saturday: Mainly clear and dry with light winds and 1200m freezing levels.

Avalanche Summary

Observations from Tuesday are limited due to poor visibility. Reports include one natural cornice triggered Size 2.5, 100cm thick wind slab avalanche on a north aspect. One recent Size 3 glide slab avalanche was also observed on a south aspect at 1800m.

Snowpack Summary

Another 10-40cm during the day and overnight Tuesday added to the 30-60cm of recent storm snow. Sustained southeasterly through northeasterly winds contributed to continued wind slab formation at all elevations, as well as cornice development. Although generally settling and bonding well, recent snowpack tests on a north facing treeline slope resulted in easy to moderate shears down 25cm within the storm snow, and down 65cm on an underlying crust. Not only will daytime warming and sun-exposure cause surface snow to lose cohesion and cornices to weaken, they will also increase settlement rates and decrease slab stability.

Regioni coperte