Boletín de aludes

Kootenay Boundary

Apr 16 – 17, 2018Avalanche Canada
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Archivado · caducó 8 years ago

Peligro de aludes

Wed
Thu
Alta montaña
3 · Notable
Límite del bosque
3 · Notable
Bajo el límite
3 · Notable
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Lo esencial

More snow is expected on Tuesday. Observe for the bond of the new snow to the previous surfaces before committing into avalanche terrain. Be particularly cautious under periods of rapid snowfall loading, as avalanche activity will likely increase.

Problemas de aludes

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2.5
    20 to 30 cm of snow fell on Monday, producing slabs that may not bond well to previous surfaces, including wet snow at low elevations, a crust at higher elevations, and wind slabs near ridge tops. More snow on Tuesday will make the slabs touchier.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2.5
    Precipitation will fall as rain at low elevations. The snow will rapidly weaken and could slide easily with the weight of a human, producing large avalanches.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

TUESDAY: Cloudy with snowfall, accumulation 10 to 20 cm, light to moderate west winds, alpine temperature -3 C, freezing level 1500 m.WEDNESDAY: Mostly sunny and afternoon clouds, light southeast winds, alpine temperature -3 C, freezing level 1500 m.THURSDAY: Mostly sunny, light southwest winds, alpine temperature 0 C, freezing level 2000 m.

Avalanche Summary

On Sunday, many loose wet avalanches and storm slab avalanches were triggered naturally and by explosives.  They were large (size 2 to 2.5) and on all aspects between 1700 m and 2100 m. 

Snowpack Summary

Around 20 to 30 cm of snow fell on Monday.  This fell on moist snow or a melt-freeze crust up to at least 1800 m produced from rain and warm temperatures on Sunday.  Numerous other melt-freeze crusts exist in the upper snowpack from rain, sun, and warming during the spring season. The snowpack below this is generally well-settled and strong.At lower elevations below treeline, a spring snowpack exists.

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