Bollettino valanghe

South Coast

Feb 13 – 14, 2014Avalanche Canada
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Archiviato · scaduto 13 years ago

Pericolo valanghe

Sat
Sun
Alta quota
4 · Forte
Limite del bosco
3 · Marcato
Sotto il limite
3 · Marcato

In sintesi

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    1–5
    A touchy and destructive storm slab, which has shown reactivity at all elevation bands, sits over a variety of potentially weak surfaces which formed during the recent cold snap. Conservative terrain selection has become critical.

Confidence

Fair - Forecast snowfall amounts are uncertain on Friday

Weather Forecast

Friday: Moderate to locally heavy snowfall / Strong southwest winds / Freezing level at 500mSaturday: Light snowfall becoming moderate to heavy overnight / Strong southwest winds / Freezing level at 800mSunday: Light snowfall / Strong southwest winds / Freezing level at surface

Avalanche Summary

Widespread storm slab avalanche activity to size 2.5 was observed throughout the region on Wednesday. Avalanches were triggered naturally or remotely by skiers, and occurred on a variety of aspects and at all elevation bands.

Snowpack Summary

Between 55cm (in the north of the region) and 90cm (along the Coquihalla) of recent snowfall overlies a medley of old surfaces buried on February 10th. These layers include: weak surface facets, surface hoar, a scoured crust, or any combination thereof. Professionals are expressing particular concern for the combination of buried facets on a crust being unusually reactive at lower elevations. Reports of whumphing and widespread avalanche activity further indicate a poor bond between the new snow and these old surfaces. Strong to extreme winds are shifting the new snow into deeper, reactive wind slabs in exposed terrain. With forecast warming and more snow on the way, the reactivity and destructive potential of the new storm slab will likely increase.The mid and lower snowpack are generally strong and well-settled. Although basal facets and depth hoar are likely to exist in the north of the region, but triggering has become unlikely.

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