Boletín de aludes

South Rockies

Feb 23, 2019Avalanche Canada
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Archivado · caducó 8 years ago

Peligro de aludes

Sun
Mon
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Lo esencial

New snow will be adding to our wind slab problems at upper elevations over Friday night. Meanwhile, riders can still trigger persistent weak layers at lower elevations. Terrain like cutblocks, steep forest openings, and gullies remain suspect.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–2
    Light new snow amounts will be resupplying our already active wind slab problem over Friday night. Winds are set to shift from southwest to east, so touchy new slabs may be expected on a variety of aspects.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1.5–2.5
    A weak layer of surface hoar is buried around 50 to 80 cm, which is best preserved in shaded and sheltered areas between 1600 m and 1900 m.

Confidence

Moderate -

Weather Forecast

Friday night: Mainly cloudy with scattered flurries bringing a trace to 5 cm of new snow. Light to moderate southwest winds.Saturday: Mainly cloudy with isolated flurries and a trace of new snow. Light to moderate northeast winds. Alpine high temperatures around -16.Sunday: Sunny with cloudy periods. Light variable winds. Alpine high temperatures around -18.Monday: Cloudy with sunny periods. Light to moderate east winds increasing over the day. Alpine high temperatures around -15.

Avalanche Summary

Several large (size 2) wind slabs were triggered with explosives control in the Castle area on Friday after a bout of strong to extreme southwest winds. Slab depths ranged from 20-60 cm.A MIN report from Grizzly Peak in the Elkford area on Thursday describes a persistent slab failing on the mid-January persistent weak layer as a ski touring group ascended a steeper slope near treeline. See the report here: LINK On Thursday in adjacent Waterton National Park a recent large (size 2) deep persistent slab avalanche was observed. It occurred on a steep feature below treeline that was noted for its thin snowpack and for being reverse loaded by winds.

Snowpack Summary

Wind slabs exist in open, exposed areas at higher elevations. They may be found on all aspects due to variable wind directions. In sheltered terrain, around 20 to 30 cm of recent soft snowfall may be found.The mid-January weak layer of surface hoar or faceted grains is buried around 50 to 80 cm. It is found on shaded and sheltered slopes and is most prominent between 1600 m and 1900 m but has been found up to 2200 m. It may overly a melt-freeze crust on south aspects. Recent avalanche reports and snowpack test results suggest that this layer remains reactive to human triggers.The middle of the snowpack is generally consolidated. The bottom half of the snowpack is unconsolidated and composed of weak and sugary faceted grains. There is potential for shallower avalanches to step down to these deeper weak layers.

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