Bollettino valanghe

Northwest Coastal

Feb 25 – 26, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

Wed
Thu
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
2 · Moderato

In sintesi

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–5
    It may be possible to trigger deep storm slabs in steep terrain, particularly in exposed lee and cross-loaded features (north through east facing slopes).
  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–5
    Cornices have grown large and weak and may pop off with continued growth or during periods of mild sunny weather.

Confidence

Fair - Forecast snowfall amounts are uncertain

Weather Forecast

Synopsis: A frontal system will hit the coast early on Tuesday spreading moderate snow and increasing winds. This is followed closely by a second system late Wednesday.  Tuesday: Light to moderate snowfall – 10-15 cm. The freezing level is around 600 m and winds increase to very strong from the south-southeast. Wednesday: Unsettled with light snow during the day and heavier snow in the evening (~15 cm). The freezing level is steady near 600-700 m and winds remain strong from the south-southwest. Thursday: Moderate to locally heavy snow. The freezing level climbs closer to 1000 m.

Avalanche Summary

Better weather on Sunday allowed for more observations of a fairly widespread natural avalanche cycle in higher alpine terrain. Slabs were reported to be size 2-3 and were primarily from wind loaded features. On Sunday, the storm and wind slabs were still reactive to ski cuts to size 1.5 and explosive control to size 3. Loose moist avalanches were also observed on steep southerly aspects when the sun came out.

Snowpack Summary

Mild temperatures have promoted rapid settlement of the recent storm snow. Strong southwest winds also created deep and weak wind slabs in exposed lee terrain and cross-loaded gully features. This new snow fell on a crust, old wind slab, and/or surface hoar depending on aspect and elevation. One recent snowpack test near Shames resulted in a hard "pops" shear on the buried surface hoar, down around 60 cm at the time. Most areas are reporting that the snow has bonded well to the underlying melt-freeze crust. Cornices that now loom over many features may become weak with continued growth and/or daytime warming. The mid and lower snowpack layers are generally well settled and strong. The exception seems to be the Bear Pass area where basal facets are still reported.

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