Bollettino valanghe

Sea To Sky

Apr 3 – 4, 2012Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

Thu
Fri
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
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 - Likely
    Dimensione
    1–5
    Generally lurking below ridgecrests, behind terrain features, and in gullies. Thick fresh wind slabs are highly sensitive to human triggers and cornice falls.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–6
    Cornices are very large and probably unstable. Not only are they a hazard in themselves, but can also act as a heavy trigger for very large avalanches on the slope below.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–6
    Storm slabs could be sensitive to human triggers and have the potential to step-down to deeper weaknesses buried last week resulting in highly destructive avalanches.

Confidence

Good

Weather Forecast

Unsettled conditions in the wake of Tuesday's storm system are expected to produce cloudy conditions and isolated light flurries with a few centimetres each day for the forecast period. The freezing level is expected to drop to and remain around 800 m, and the winds should remain light and variable.

Avalanche Summary

Reports from Monday include numerous soft wind slab avalanches up to size 1.5 occurring naturally as well as with direct and remote human triggers. Sustained heavy loading from snow wind and rain on Tuesday likely resulted in continued natural avalanche activity particularly on lee slopes.

Snowpack Summary

As of Tuesday morning heavy snowfall has already deposited up to 50cm, which is being redistributed by strong southwesterly winds into thick wind slabs. These wind and storm slabs are poorly bonded and continued snowfall and wind is adding additional load. A predominately crusty weak interface from late March, now down 50-150cm, remains a potential failure layer for large slab avalanches, especially with heavy triggers such as cornice falls and step-down avalanches. Cornices are also huge and weak.

Regioni coperte