Bulletin d’avalanche

Kootenay Boundary

Jan 29 – 30, 2015Avalanche Canada
Voir sur la carte
Archivé · expiré 12 years ago

Danger d’avalanche

Sat
Sun
Alpin
2 · Modéré
Limite forestière
2 · Modéré
Sous la limite
1 · Faible

Points saillants

The cooling trend continues to reduce the avalanche danger.

Problèmes avalancheux

  • Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    2–4
    Strong solar radiation may result in natural avalanches releasing on the buried persistent weak layer on Southerly aspects. Avalanches may be human triggered on all aspects.
  • Loose Wet

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    1–2
    Moist or wet loose snow is expected to continue to release from light additional loads, or from strong solar radiation on Southerly aspects. 

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

The freezing level is expected to drop down to valley bottoms overnight and then rise up to about 900 metres on Friday. Friday should be mostly sunny with valley cloud and light winds. There is a chance of a weak above freezing level in the alpine between 2000 – 2500 metres during the day. Saturday should be a mix of sun and cloud with valley cloud persisting and winds becoming moderate from the Northwest. Precipitation is expected to start early Sunday morning and continue during the day with 5-10 mm forecast.

Avalanche Summary

There are no new reports of avalanches. On Monday there were several size 2.0-2.5 loose wet and wet slab avalanches released with explosives at Kootenay Pass, and a size 3.0 natural avalanche in the backcountry near Whitewater ski resort on a Southeast aspect with a very wide propagation that probably released on the mid-January persistent weak layer during a period of strong solar radiation. Moist or wet loose snow avalanches have been reported from several areas up to size 2.0 over the past few days during the warming event. On Saturday a skier triggered a size 2 persistent slab which failed on the mid-December layer. This was a surprising result because it was on a well-supported, concave terrain feature (which had also been heavily skied).

Snowpack Summary

The cool down has started. Overnight freezing down to valley bottoms has created melt-freeze crusts. Strong solar radiation and warm temperatures are affecting the surface layers and turning them moist or wet. We are in a spring like diurnal freeze/thaw cycle. Periods of warming has increased the likelihood of triggering the persistent weak layer of mid-Jan surface hoar layer which is down about 20-60 cm. These large, well-preserved surface hoar crystals sit on a thin crust up to about 1900m on north aspects and all the way to ridgeline on south aspects. A deeper crust/surface hoar combo buried in mid-December is typically down 80-120cm and has produced some large avalanches recently.

Régions couvertes