Boletín de aludes

Kispiox

Jan 3 – 4, 2026Avalanche Canada
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Archivado · caducó 9 months ago

Peligro de aludes

Mon
Tue
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Snowpack modelling suggests a dangerous weak layer can be triggered.

Watch for whumpfing and signs of instability.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–2.5

    Strong southerly winds and soft surface snow have created wind slabs. Avoid wind loaded features.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–3

    A dangerous weak layer of sugary facets is suspected around 50 cm deep, additionally, in areas with less than 120 cm of snow the base of the snowpack may be unstable.

Confidence

Low

  • Uncertainty is due to limitations in the field data.

Avalanche Summary

On Wednesday, a small natural wind slab occurred on a steep northeast aspect in the alpine.

No other avalanches have been reported since then, however, reports are very limited.

Snowpack Summary

15 cm of snow fell earlier in the week with warm temperatures and strong southerly winds. This likely sits on a layer of small facets. Lower elevations may have a crust on the surface.

Areas with less than 120 cm of snow may have a concerning weak layer at the base of the snowpack.

Weather Summary

Friday Night
Partly cloudy. 2 cm of snow. 10 km/h south ridgetop wind. Treeline temperature -13 °C.

Saturday
Mix of sun and clouds. 1 cm of snow. 10 km/h southeast ridgetop wind. Treeline temperature -12 °C.

Sunday
Mix of sun and clouds. 10 km/h south ridgetop wind. Treeline temperature -13 °C.

Monday
Mix of sun and clouds. 2 to 5 cm of snow. 20 km/h southwest ridgetop wind. Treeline temperature -16 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be aware of the potential for large avalanches due to buried weak layers.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

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