Bollettino valanghe

Purcells

Jan 3, 2018Avalanche Canada
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Archiviato · scaduto 9 years ago

Pericolo valanghe

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

In sintesi

Warming alpine temperatures may give some surprising releases, especially in steep terrain.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Wind slabs have been reported and are likely to continue to develop in exposed terrain. Warmer temperatures at higher elevations may also make the upper snowpack denser.
  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    A weak layer of surface hoar buried 30-50 cm deep is expected to become more reactive as warmer temperatures help settle recent new snow into a cohesive slab.

Confidence

Moderate - Timing or intensity of solar radiation is uncertain

Weather Forecast

Wednesday: Cold air in the valleys, warmer air up high that is expected to get close to 0C above 2200m. Some valley cloud is possible, clear at upper elevations. Light variable winds.Thursday: Clear in the morning, cloud developing through the day. Inversion conditions expected to persist. Moderate southwesterly winds.Friday: Cloudy with some flurries. Freezing level creeping up to around 1000 m. Some warm air remaining at higher elevations. Moderate southwesterly winds

Avalanche Summary

On Sunday, a size 1.5 avalanche involving two people near Invermere was reported. It was suspected to have run on the mid-December weak layer. On Saturday a skier triggered size 2 persistent slab avalanche running on a layer of facetted snow from mid-December was reported. This happened in the north of the region's Dogtooth Range on a west aspect at 2400m. Expect the potential to trigger persistent slabs to increase as last week's storm snow continues to settle into a cohesive slab.

Snowpack Summary

20-40 cm low density new snow has accumulated and buried a recently formed layer of weak feathery surface hoar and/or sugary facets. Another layer buried mid-December that consists of surface hoar, sun crust and/or sugary facets is down approximately 40-70cm and has been reported at elevations up to 2400 m. The likelihood of triggering avalanches on either of these layers is related to how dense the upper snowpack is. In areas where the upper snowpack has settled into a firmer slab, the weak layers below are more likely to be triggered. A rain crust that formed in late November is now buried 70-110cm deep. Recent reports show this layer to be unreactive at this time.

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