Bollettino valanghe

Cariboos

Feb 21 – 22, 2012Avalanche Canada
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Archiviato · scaduto 15 years ago

Pericolo valanghe

Thu
Fri
Alta quota
4 · Forte
Limite del bosco
4 · Forte
Sotto il limite
3 · Marcato

In sintesi

Conditions are primed for widespread avalanche activity. Conservative decision making is essential for safe backcountry travel at this time.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Very Likely
    Dimensione
    1–5
    Strong west-northwest winds will continue to build deep windslabs overlying several persistent weaknesses in the upper snowpack.
  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Very Likely
    Dimensione
    1–4
    Up to 60cm of settling storm snow overlies several weaknesses including surface hoar and a sun crust. Forecast snow and wind may overload this weakness causing a widespread avalanche cycle on Wednesday.

Confidence

Good

Weather Forecast

Tonight and Wednesday: Moderate snowfall with 10-15cm likely overnight, and an additional 5cm on Wednesday. The freezing level (FL) drops overnight to 500-700m. Strong westerly winds overnight shifting to moderate-strong from the northwest on Wednesday afternoon. Thursday: Mainly dry under a weak ridge of high pressure. FL near valley bottom. Friday: Light snowfall - around 5cm. FL at valley bottom. Winds should be moderate from the southwest.

Avalanche Summary

There are several reports of natural and skier triggered avalanches up to Size 1.5. These avalanches occurred in wind affected terrain in the alpine, or on steep convex shaped features below treeline. The size and likelihood of avalanches will increase as the new snow settles into a more cohesive slab.

Snowpack Summary

Wind slabs continue to grow in exposed terrain in response to moderate W-SW winds. 20-50cm of slowly settling storm snow overlies the Feb. 9 weakness, which includes surface hoar and/or a crust. This surface hoar layer may be widespread in some areas, while others have reported it being confined to shady aspects at treeline and in the alpine. A melt-freeze crust has developed on solar aspects at all elevations, and on all aspects below about 1600 metres. The mid-pack is generally well settled. There is some concern that large loads like cornices may trigger the Jan. 20th facet layer. Some shallow snowpack areas may continue to have a weak layer of basal facets near the ground.

Regioni coperte