Bollettino valanghe

Northwest Coastal

Mar 17 – 18, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

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

In sintesi

Problemi valanghivi

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    2–6
    Cornices are reported to be large and unstable, especially when temperatures become warm or the sun is out. Watch for reverse loading from outflow winds.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–5
    Recent new snow has consolidated into a slab and is reacting on steep terrain. Outflow winds have reverse-loaded slopes in some areas. The underlying weak layer of surface hoar is quite touchy.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Synopsis: Northwest flow gives way to a frontal system that barely brushes the region on Tuesday night/Wednesday.Monday: Flurries, with some breaks in the cloud giving daytime warming. Afternoon freezing level around 500 m. Winds light northwesterly.Tuesday: Light snow starting late in the day. Freezing level 500 m. Southerly ridgetop winds increasing to around 50 km/h.Wednesday: 5-10 cm new snow. Freezing level 500 m. Winds light southeasterly.

Avalanche Summary

On Saturday, natural slab avalanches were reported up to size 3 on all aspects in the alpine. Solar aspects were particularly reactive and daytime warming triggered slides on the surface hoar layer from March 9th buried approximately 45 cm. Cornice releases were also numerous and triggered slab avalanches on the slopes below. On Friday, a skier triggered a size 2 avalanche on the March 9th surface hoar layer with a crown depth of 45 cm. Several other skier-triggered avalanches occurred on north and west aspects on the same weak layer.

Snowpack Summary

25-50 cm of recent storm snow rests on a variety of old snow surfaces, including crusts, previous wind slabs and surface hoar. Warmer temperatures and recent winds have now set this new snow into a reactive slab, with wind slabs building in exposed lee areas. The surface hoar (buried March 9th) is reported to be well-developed and fairly widespread, at treeline and alpine elevations. Recent snowpack tests have produced sudden failures with moderate loading force at this interface. The mid snowpack is generally well settled and strong. Cornices are large and untrustworthy, especially when the sun is out.

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