Bollettino valanghe

Sea To Sky

Apr 6 – 7, 2017Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 9 years ago

Pericolo valanghe

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

In sintesi

Yet another Pacific frontal system will impact the region keeping the avalanche danger elevated

Problemi valanghivi

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–3
    Large cornices may become weak with daytime warming or during periods of stormy weather.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    The combination of new snow, moderate to strong southerly winds and warm temperatures have created reactive storm slabs. These are expected to especially touchy in the lee of exposed terrain features.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Friday

Weather Forecast

FRIDAY: Periods of snow, accumulation 15-25cm / Moderate to strong south wind / Alpine temperature -3 / Freezing level 1600mSATURDAY: Mainly cloudy with isolated flurries, accumulation 5-10cm / Moderate southwest wind / Alpine temperature -6 / Freezing level 1300mSUNDAY: Mainly cloudy / Light south wind / Alpine temperature -8 / Freezing level 900m

Avalanche Summary

Reports from Wednesday include explosives triggered storm slabs running to size 2, 30cm deep. On Monday a few natural cornice releases to size 2.5 were observed running to the bottom of their run outs entraining loose snow only. On Sunday, a natural cornice release triggered a size 3 slab avalanche which release down 60 cm and ran to valley bottom. On Friday, expect newly formed wind and storm slabs to be reactive to human triggering. These slabs are expected to be particularly touchy where they overlie a melt-freeze crust.

Snowpack Summary

25-40cm of new snow at upper elevations sits on widespread melt-freeze crusts on all aspects and elevations except for high elevation north facing terrain. On all aspects below 2000 m and higher on sun exposed slopes, there may be multiple crust layers in the upper snowpack. Moderate to strong alpine wind from the south will have redistributed this new snow and formed additional wind slabs in the alpine and at tree line which may overlie a crust. Large overhanging cornices exist primarily on north aspects in the alpine.

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