Boletín de aludes

Northwest Inland

Feb 14, 2019Avalanche Canada
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Archivado · caducó 8 years ago

Peligro de aludes

Fri
Sat
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil
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Lo esencial

Recently formed small wind slabs at higher elevations may remain reactive to human triggering. Sheltered lower elevations are likely to still hold the best skiing and riding conditions.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–2
    Relentless outflow winds have been redistributing snow at higher elevations for days. There is likely a mix newer, smaller, more reactive wind slabs as well as older, larger, more stubborn slabs to be found in wind-affected areas.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Wednesday night: Cloudy with clear periods. Light to moderate southeast winds, increasing overnight.Thursday: Cloudy with sunny periods. Moderate to strong southeast or east winds. Alpine high temperatures around -14.Friday: Mainly cloudy with isolated flurries and a trace of new snow. Light east winds. Alpine high temperatures around -21.Saturday: Sunny with cloudy periods. Light northeast winds. Alpine high temperatures around -21, increasing overnight.

Avalanche Summary

Winds have been driving avalanche danger at higher elevations, redistributing recent snow accumulations into wind slabs. Skiers reported small natural wind slab releases, whumpfing, and shooting cracks on Thursday and Friday. A small (size 1) ski cut wind slab at 2100 metres was reported on Sunday. Most wind slabs are likely to be stabilized at this point, however, more recent small slabs in steep leeward features still need to be considered and managed.

Snowpack Summary

In the alpine and upper treeline, the upper snowpack is composed of successive layers of aging, wind-affected storm snow layers. The most recent wind slabs are likely to exist on on southwest aspects as a result of ongoing, predominantly northeast winds. The upper snowpack has also been faceting (becoming sugary) under the influence of recent cold temperatures at all elevations.Sheltered areas at lower elevations still hold around 20-30 cm of low density snow from a couple of recent snowfall events. Below this more recent snow, another 20-40 cm of older, faceted (sugary) storm snow overlies a widespread melt-freeze crust. In the central and northern parts of the region, it may sit on feathery surface hoar crystals in sheltered terrain at all elevations. In the south of the region, the remainder of the snowpack has been reported as well-settled.Around and north of Hazelton, 50 to 100 cm of snow may overlie two weak layers of surface hoar or sugary faceted grains.

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