Boletín de aludes

Kootenay Boundary

Jan 31, 2017Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

Tue
Wed
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Watch for changing conditions at higher elevations and be cautious around thin rocky areas where wind slabs could step down to deeper weak layers. Thanks to everyone who's shared observations on the MIN!

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Watch for pockets of wind slabs on exposed features near ridge crests and cross-loaded gullies. Also be cautious around thin rocky areas where wind slabs could 'step down' to deeper weak layers.

Confidence

Moderate - The weather pattern is stable

Weather Forecast

TUESDAY: Sunny with cloudy periods, light east winds, alpine temperatures around -10 C.WEDNESDAY: Sunny with cloudy periods, light east winds, alpine temperatures around -12 C.THURSDAY: Sunny, light east winds, alpine temperatures around -12 C.

Avalanche Summary

On Monday, several size 1 wind slab avalanches were skier triggered in the lee of ridgetops. Isolated natural wind slab activity in the size 1.5-2 from a few days ago was also reported. A large natural avalanche (size 2.5) was reported on a wind-loaded east facing slope in the Rossland range. This avalanche likely released on a deeper persistent weak layer.Expect wind slabs to linger on lee and crossloaded features at higher elevations.

Snowpack Summary

A variety of surface conditions exist including wind affected snow, sun crusts, shallowly buried surface hoar, and pockets of light snow. A total of 30-50 cm of settled snow now sits above a weak interface that was buried in mid-January. The interface is composed of weak facets, surface hoar, and/or sun crusts. The strength of this interface is variable, but has continued to give some sudden results and propagations in snowpack tests. Areas with thin snowpacks (e.g. less than 150 cm) have a generally weak snowpack structure with sugary facets near the ground. This includes shallow alpine slopes and most of the Rossland range. These deeper weaknesses warrant long term monitoring, as they could reawaken with a sudden change in the weather.

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