Bollettino valanghe

Cariboos

Jan 31 – Feb 1, 2023Avalanche Canada
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Archiviato · scaduto 4 years ago

Pericolo valanghe

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

In sintesi

6:15 AM Update: A natural avalanche cycle is expected. Travel in avalanche terrain is not recommended.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    1–2

    New snow and strong westerly wind are forming new wind slabs in lee terrain features. Storm slabs may also build in wind-sheltered terrain. The new snow may overly lingering wind slabs that formed on the weekend from northeast wind.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–3

    Two surface hoar layers found 30 to 80 cm deep have been reactive in scattered areas around the region. Be especially cautious around steep openings within and near treeline elevations.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2.5–4

    A layer of large and weak facets sits near the base of the snowpack. This layer continues to produce very large avalanches that can travel far. The likelihood of natural and human-triggered avalanches will increase as snow accumulates. Riders are most likely to trigger an avalanche on this layer in steep, shallow terrain, or by triggering a smaller avalanche that could step down to this layer.

Confidence

Moderate

Avalanche Summary

On Sunday, several large to very large (size 3 to 4) avalanches were triggered naturally on the basal facets. The avalanches were on all aspects and generally in alpine terrain between 2400 and 2900 m. See here for a video of a rider-triggered avalanche near Renshaw and another example here near Clearwater. Numerous shallower wind slabs were also triggered in alpine terrain.

These avalanches are similar to what we've seen over the past week, with persistent and deep persistent avalanches releasing on all the weak layers described in the Snowpack Summary. Most avalanches over the past week were large to very large (size 2 to 4), occurring between 1700 and 2400 m and on all aspects. See this MIN for a recent example and see here for information on a fatal skier-triggered avalanche incident from last week near Revelstoke.

See more on the potential of triggering deeper weak layers Forecasters' Blog.

Snowpack Summary

New snow and strong westerly wind will form new wind slabs in lee terrain features. They will overly previously wind-affected snow from recent northeast wind. Storm slabs may begin to form in wind-sheltered terrain.

Two layers of surface hoar crystals and/or a melt-freeze crust may be found around 30 to 80 cm deep. Surface hoar is most likely found in wind-sheltered terrain around treeline and lower alpine elevations. The melt-freeze crust is found up to 1800 m on all aspects and into the alpine on sun-exposed slopes.

Large and weak facets from November are near the base of the snowpack, which continue to produce very large avalanches in the region.

Weather Summary

Monday Night

Cloudy with snowfall, accumulation 5 to 15 cm with local enhancements possible, 20 to 30 km/h west wind, treeline temperature -12 °C.

Tuesday

Cloudy with snowfall, accumulation 5 to 15 cm with local enhancements possible, 20 to 40 km/h west wind, treeline temperature -12 °C.

Wednesday

Cloudy with snowfall, accumulation 10 to 20 cm with local enhancements possible, 20 to 40 km/h southwest wind, treeline temperature -10 °C.

Thursday

Cloudy with snowfall, accumulation 5 to 10 cm, 30 to 40 km/h southwest wind, treeline temperature -6 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Travel in alpine terrain is not recommended.
  • Avoid exposure to overhead avalanche terrain, avalanches may run surprisingly far.
  • Wind slabs are most reactive during their formation.
  • Be mindful that deep instabilities are still present and have produced recent large avalanches.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
  • Surface hoar distribution is highly variable. Avoid generalizing your observations.

Regioni coperte