Boletín de aludes

South Columbia

Apr 15 – 16, 2017Avalanche Canada
Ver en el mapa
Archivado · caducó 9 years ago

Peligro de aludes

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

Lo esencial

Falling cornices continue to trigger large avalanches. Solar radiation and rapidly rising freezing levels make this a very real possibility on Sunday.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–2
    Convective flurries and moderate southwesterly winds have created wind slabs in lee features at treeline and above that were reactive to human triggers on Saturday.

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–4
    Avoid all slopes that are threatened by cornices on Sunday.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2
    Small loose wet avalanches have the potential to trigger large avalanches on sugary facets near the bottom of the snowpack.

Confidence

High -

Weather Forecast

SUNDAY: Sunny. Light southerly ridgetop winds. Freezing level RAPIDLY RISING to 2000m.MONDAY: Mix of sun and cloud with isolated flurries. Light southwesterly ridgetop winds. Freezing level hovering around 1900m.TUESDAY: Cloudy with light rain/snow. Light southerly ridgetop winds. Freezing level around 1900m.

Avalanche Summary

Two skier triggered wind slabs up to size 1.5 were reported in this region on Friday. The key weather factor to keep your eye on this weekend will be the sunshine accompanied by rising freezing levels. These are common trigger for cornices which is currently our primary concern due to their ability to trigger large avalanches.

Snowpack Summary

Cornices are large, looming, and the primary concern due to their potential to trigger large avalanches failing on facets at the bottom of the snowpack. Convective showers and moderate southwesterly winds have formed small wind slabs on lee features below ridgetops. Solar radiation is a common trigger for loose wet avalanching in steep terrain, especially when new snow gets heated by the sun for the first time.

Regiones cubiertas