Boletín de aludes

Cariboos

Apr 24 – 25, 2025Avalanche Canada
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Archivado · caducó last year

Peligro de aludes

Sat
Sun
Alta montaña
1 · Débil
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil

Lo esencial

Avoid travelling underneath cornices.

As the crust breaks down, reduce your exposure to avalanche terrain.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1.5–2.5

    Cornices are more likely to fail during warm weather.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–1.5

    Wet loose avalanches will become more likely as the sun and warmth affect the snowpack. Start early, and avoid the hottest part of the day.

Confidence

Moderate

Avalanche Summary

On Wednesday, there was a large cornice failure that triggered a wet loose avalanche out of extreme terrain.

Observations are limited at this time of year.

Snowpack Summary

A thin cust is likely to have formed over up to 20 cm of recent snow at upper elevations. This snow overlies a robust crust everywhere except northerly aspects in the alpine.

Most terrain has undergone strong melt-freeze cycles, creating a strong, well bonded snowpack.

Weather Summary

Thursday Night

Partly cloudy. 20 to 30 km/h southeast ridgetop wind. Treeline temperature 1 °C. Freezing level 2200 m.

Friday

Mix of sun and clouds. 20 to 40 km/h southwest ridgetop wind. Treeline temperature 5 °C. Freezing level 2300 m.

Saturday

Mix of sun and cloud. 10 to 20 km/h west ridgetop wind. Treeline temperature 4 °C. Freezing level 2100 m.

Sunday

Mix of sun and cloud. 10 km/h variable direction ridgetop wind. Treeline temperature 0 °C. Freezing level 1800 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid steep, sun-exposed slopes when the air temperature is warm or when solar radiation is strong.
  • Avalanche danger will increase as the surface crust breaks down.

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