Bollettino valanghe

Lizard-Flathead

Dec 4, 2017Avalanche Canada
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Archiviato · scaduto 9 years ago

Pericolo valanghe

Tue
Wed
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

Recent storm snow accumulations are up to 50 cm. Storm slabs may be reactive to rider triggers. With limited observations and a variable snowpack use a conservative approach to route selection and terrain with low consequence.

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Storm slabs may have a poor bond to a buried crust down 30-60 cm and could be reactive to rider triggers. Dry loose avalanches may be able to push you into terrain features that have consequence.

Confidence

Low - Due to the number and quality of field observations

Weather Forecast

Monday: Mix of sun and cloud. Alpine temperatures near -10 and freezing levels at valley bottom. Ridgetop winds light from the west.Tuesday: Cloudy with sunny periods. Alpine temperatures near -8 and freezing levels at valley bottom. Ridgetop winds light from the west.Wednesday: Mix of sun and cloud. Alpine temperatures high of 0 degrees with freezing levels at valley bottom. Strong alpine temperature inversion.Expect strong inversions in the alpine up to 3000 m by Thursday. For detailed information visit the Mountain Weather Forecast.

Avalanche Summary

On Sunday, avalanche control with explosives triggered numerous size 1 dry loose avalanches above 1900 m from northeast aspects. Reactive storm slabs and dry loose avalanches may persist through Tuesday. Please submit your observations this weekend to the Mountain Information Network. Give info, get info.

Snowpack Summary

Up to 50 cm of accumulated storm snow has fallen on the crust that formed a week ago. The buried crust is supportive and approximately 10 cm thick. It extends from 1600 m to mountain top elevations on all aspects. Lots of uncertainty exists with the new snow sticking to the crust. Winds are likely redistributing the new snow above treeline and possibly forming wind slabs on leeward slopes and terrain features. The average snowpack depth at treeline is 60-80 cm while a deeper snowpack exists in the alpine.

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