Bulletin d’avalanche

Chic-Choc Mountains

Mar 7 – 8, 2025Avalanche Canada
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Archivé · expiré 2 years ago

Danger d’avalanche

Sun
Mon
Alpin
3 · Marqué
Limite forestière
3 · Marqué
Sous la limite
2 · Modéré

Points saillants

Weather models disagree on the amount of snow expected between Friday evening and Saturday evening. Be careful: the snow that falls after the rain episode may not adhere well to the old snow.

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely
    Taille
    1–2

    There is a great deal of uncertainty about the amount of snow that will fall in the mountains and its cohesion with the snow already present. Beware of snow recently carried by the wind.

Confidence

Low

Avalanche Summary

Few observations in the field today. No new avalanches were observed or reported.

If you are out in the backcountry, please share your observations on the Mountain Information Network (MIN).

Snowpack Summary

Saturday morning, between 10 and 25 cm of new snow will cover wet snow and/or crust. New snow accumulation will be greatest at higher altitudes. Snow cover in the alpine is likely to have diminished considerably due to extreme southerly winds, rain and recent high temperatures.

The height of the snowpack varies between 100 cm and 200 cm.

Weather Summary

WEATHER FOR THE CRESTS AND SUMMITS OF CHIC-CHOCS

From Friday afternoon to Saturday morning, heavy snow is expected, followed by persistent blowing snow until Saturday night.

Friday evening and night: Snow, sometimes heavy. Accumulations of 10 to 15. Winds west, 20 to 40 km/h. Minimum -14 °C.

Saturday: Intermittent snow. Accumulation of 4 to 8 cm. Wind west, 40 to 60 km/h. Maximum -12 °C.

Sunday: Alternating sun and clouds. Accumulation of 3 to 5 cm. Northwest winds, 30 to 50 km/h. Maximum -10 °C.

Monday: Alternating sun and clouds. Wind northwest, 20 to 40 km/h. Maximum -10 °C.

For more details, see the Chic-Chocs alpine weather forecast.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.

Régions couvertes