Bollettino valanghe

Purcells

Mar 14 – 15, 2016Avalanche Canada
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Archiviato · scaduto 11 years ago

Pericolo valanghe

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

In sintesi

As stormy weather tapers-off and a dry ridge gradually builds over the province, solar radiation may become the driver for natural avalanche activity.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Recently formed wind slabs may remain sensitive to light inputs in higher elevation lee terrain. Brief periods of solar radiation may also promote loose wet avalanche activity on steep, sun-exposed slopes.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–4
    Large cornices loom over open bowls and alpine faces. Not only are massive cornice falls a hazard in themselves, they can also act as a heavy trigger for slab avalanches on the slope below.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    3–5
    A persistent weak layer continues to produce intermittent large avalanches. Although this layer is slowly becoming less likely to trigger, it has the potential to surprise with nasty consequences. I'd continue riding with a conservative mind set.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Light snowfall (2-3cm) is expected on Tuesday and early Wednesday. Clouds are expected to scatter throughout the day on Wednesday, while clear skies are forecast for Thursday. Ridgetop winds are expected to be generally light to moderate and southwesterly on Tuesday, switching to northwesterly by Wednesday. Daytime freezing levels should hover around 1200m for the forecast period.

Avalanche Summary

A natural wind slab avalanche cycle to size 2.5 was observed in mostly northeast facing alpine terrain on Sunday. The activity occurred in response to new snow and strong southwest winds on Saturday night. A size 2 persistent slab avalanche was also noted on Sunday in the Dogtooth Range. The avalanche, which failed on a northeast aspect at 2200m, started as a smaller wind slab and stepped-down to the late February layer. On Monday, explosives control triggered another size 2 persistent slab avalanche on a north facing alpine slope.

Snowpack Summary

On Saturday night, 8-15cm of new snow fell. Strong southwest winds redistributed these accumulations into touchy wind slabs at treeline and in the alpine. 35-70 cm below the surface you'll find a persistent weak layer comprised of surface hoar, facets and/or a thick crust. This layer, which was buried on February 27th, seems variably reactive. In other words, it's still really touchy in some places while in other places it's really tough to trigger, and there's not much of a reliable pattern telling us what exact aspects are most suspect. I'd continue to be suspicious of steep, unsupported features at treeline and in the alpine as this layer has the potential for large avalanches. Deeper weak layers from mid-February and early January are now down 50-90cm and 70-120cm respectively. Triggering an avalanche on either of these layers has become unlikely but either still has the isolated potential to produce very large avalanches with a heavy trigger or significant warming.

Regioni coperte