Boletín de aludes

North Columbia

Apr 18 – 19, 2024Avalanche Canada
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Archivado · caducó 2 years ago

Peligro de aludes

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

The upper snowpack will weaken throughout the day due to warming and solar radiation, while isolated slabs may persist in steep, high alpine areas.

Problemas de aludes

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2

    The upper snowpack may become unstable with daytime warming and solar effect, particularly in steep, south-facing terrain.

Confidence

High

Avalanche Summary

No recent avalanche activity has been reported.

Despite the low danger rating, the likelihood of triggering an avalanche will increase throughout the day with warming and strong solar radiation expected.

Snowpack Summary

Recent storm snow continues to settle and bond to an underlying crust. At lower elevations and south-facing slopes a surface crust will likely form overnight.

Surface snow will deteriorate and become moist throughout the day with daytime warming and strong solar effects.

Weather Summary

Thursday Night

Sunny. 0 to 20 km/h northeast ridgetop wind. Treeline temperature -6 °C. Freezing level at valley bottoms.

Friday

Sunny. 0 to 20 km/h east ridgetop wind. Treeline temperature -3 °C. Freezing level 1700 m.

Saturday

Sunny. 10 to 30 km/h southeast ridgetop wind. Treeline temperature -1 °C. Freezing level 2000 m.

Sunday

Cloudy with 0 to 10 cm of snow in alpine terrain. Treeline temperature -3 °C. Freezing level 1700 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for unstable snow on specific terrain features, especially when the snow is moist or wet.
  • Be alert to conditions that change with aspect and elevation.
  • Be alert to conditions that change throughout the day.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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