Bollettino valanghe

Sea To Sky

Dec 11, 2018Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 8 years ago

Pericolo valanghe

Wed
Thu
Alta quota
4 · Forte
Limite del bosco
3 · Marcato
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

Significant snowfall accumulation will drive up avalanche hazard.

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2.5
    The new snow is not bonding well with the old snow surface layer. More snow is on the way accompanied with strong winds. Slabs will be more prominent in wind-loaded areas, and under cornices and ridge-lines.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

MONDAY NIGHT: Flurries, accumulating up to 20 cm overnight, moderate gusting strong south wind, freezing level below 1000m. TUESDAY: Snow, accumulation 15-30 cm, moderate southwest wind with strong gusts, freezing level rising to 1400m. WEDNESDAY: Continued snow, accumulating 20-35 cm, moderate southwest wind with strong to extreme gusts, freezing level below 1000m. THURSDAY: Snow, accumulating up to 30cm, moderate southwest wind with extreme gusts, freezing level 1200m.

Avalanche Summary

The new storm snow is bonding poorly to the old surface, small (size 1) storm slabs are reacting to skier traffic around Whistler and larger avalanches (up to size 2) have been triggered by explosives. Expect avalanche activity to increase with more snow on the way along with wind.

Snowpack Summary

Snowfall beginning Sunday has added up to 30cm around the region. The weather forecast is calling for significant snowfall amounts through the week. Buried under the new snow is a weak surface layer sitting over 20-30 cm of low density faceted snow. The new snow is initially not bonding well with this old surface layer.Prior to this storm, alpine snowpack depths varied around 150-200 cm, with an early November crust at bottom of the snowpack (down 100-120cm). This crust appears to be breaking down at higher elevations and has been unreactive to snowpack tests. Snowpack depths disappear quickly with decreasing elevations (starting around 1800m).

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