Boletín de aludes

Lizard-Flathead

Dec 22, 2016Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

Thu
Fri
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado

Lo esencial

As this past week's storm snow continues to settle it will still be important to evaluate the bond between the old snow surface and the new snow. There is still potential for a week sliding layer in isolated sheltered areas.

Problemas de aludes

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Wind and warming have added cohesion to the recent storm snow, and storm slabs may be ripe for triggering. Use extra caution in steeper, wind-exposed terrain.

Confidence

Moderate - Forecast snowfall amounts are uncertain

Weather Forecast

Thursday: Mainly Cloudy / Moderate southwest wind / Alpine temperature -6Friday: Mainly cloudy with scattered flurries, accumulation 5cm / Light east wind / Alpine temperature -3Saturday: Isolated flurries/ Light north wind / Alpine temperature -8

Avalanche Summary

Numerous storm slab avalanches (mostly in the size 2 range), were observed failing naturally on Tuesday. The avalanches formed in response to heavy storm loading and failed mostly on north to northeast facing terrain at treeline and in the alpine. Looking forward, continued moderate to strong southwest winds are expected to promote ongoing wind slab activity. There is a bit of uncertainty regarding how the new snow will bond to old surfaces which formed during last week's cold snap. Due to these potentially persistent weak layers, recently formed storm slabs may remain sensitive to human triggering for some time.

Snowpack Summary

Since Sunday up to 60cm of low-density snow has fallen with the highest amounts accumulating in the Lizard Range. Strong winds and slight warming have added cohesion to the new snow and reactive storm slabs exist in wind-exposed terrain. The new snow buries a variable surface that developed over the last week of cold, dry, and windy conditions. This interface consists of scoured surfaces and wind slabs in wind exposed terrain, widespread faceting of the upper snowpack, and surface hoar up to 20 mm in sheltered areas. In sheltered areas, you may find another layer of surface hoar in the mid to upper snowpack which was buried around December 10. The mid pack is generally well settled. The thick crust from mid-November is near the bottom of the snowpack and reports suggest that the crust is currently well bonded to the surrounding snow.

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