Boletín de aludes

Kootenay Boundary

Nov 26 – 27, 2015Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Sat
Sun
Alta montaña
Sin grado
Límite del bosque
Sin grado
Bajo el límite
Sin grado

Lo esencial

Warming forecast for the next few days will increase the Avalanche Danger, especially at higher elevations. If you are out in the mountains, please post your observations to the MIN

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    Recent storm accumulations have likely been redistributed into fresh wind slabs at higher elevations. Due to the irregular loading pattern, watch for wind slabs in unsuspecting locations.
  • Loose Dry

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2
    Unseasonably warm temperatures and sun will increase the chances of loose wet avalanche activity on steep, sun-exposed slopes in the alpine and at treeline.

Weather Forecast

The dry ridge of high pressure will persist throughout the forecast period bringing clear skies at higher elevations and cloud in the valleys. A layer of warm air aloft will develop on Friday and into the weekend with above-freezing temperatures expected above 1700m. Valley temperatures should remain below freezing. Ridgetop winds will remain mainly moderate from the northeast.

Avalanche Summary

On Wednesday, ski cutting and explosives triggered several wind slab avalanches up to size 1.5. The avalanches are sliding on a firm rain crust from mid-November. Slabs were typically 5-15cm thick and were reported on a variety of aspects. These types of wind slabs may persist for a few days until temperatures warm up at higher elevations. With warming forecast for the next few days, I would add loose wet avalanche activity to the mix on steep, sun-exposed slopes .

Snowpack Summary

10-20cm of recent snowfall overlies a highly variable surface which may include surface hoar and/or facetted snow, a thick rain crust which exists to at least treeline elevation, a sun crust on steep south facing slopes, or wind-affected snow in exposed alpine terrain. At treeline elevations, the snowpack appears to typically be 1-1.5m deep. There is a thick crust from early-November in the middle of the snowpack. The limited reports we have received suggest that this crust is well bonded but you should investigate the snowpack in your local area before committing yourself to avalanche terrain. Wind slabs exist on a variety of aspects due to shifting winds and may persist for a few days.

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