Bulletin d’avalanche

Kananaskis

Apr 30 – May 1, 2019Alberta Parks
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Archivé · expiré 7 years ago

Danger d’avalanche

Thu
Fri
Alpin
Sans niveau
Limite forestière
Sans niveau
Sous la limite
Sans niveau

Points saillants

A return to wintery conditions at upper elevations requires a shift in mindset. Be prepared for wind slabs in the Alpine. Otherwise, this time of year brings rapid changes to the snowpack and avalanche hazard with solar radiation and warm temps.

Problèmes avalancheux

  • Wind Slabs

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

    Recent snow and wind have created fresh surface wind slabs in Alpine terrain. Depth of slab and bond with the underlying surface are highly variable. Dig frequently while traveling to keep a good handle on this avalanche problem.

  • Loose Wet

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

    Loose wet slides on all aspects except north aspects in the alpine should be expected when solar input is present on daytime temperatures are warm.. These loose point releases may trigger a slab on the underlying slope.

Confidence

-

Weather Forecast

A cool and snowy week is expected. Springtime squalls could deposit significant snow in certain areas, while other areas remain relatively dry. Winds will be mainly light, but localized strong gusts are possible.

Avalanche Summary

Avalanche observations are extremely limited at this time due to a lack of field observations.

Snowpack Summary

An upslope storm recently deposited 30 to 40cm of new snow on the eastern side of the range with only about 20cm on the western side. This snow is settling rapidly at lower elevations and becoming moist with daytime heating. Wind slabs are found in the Alpine on N and E aspects, and cool temperatures are generally keeping the snow dry in these areas. The bond of the new snow to the previous surfaces is highly variable, so take the time to evaluate this interface before committing to bigger terrain. Despite the recent snow and cool temperatures the snowpack is generally a springtime snowpack, with rapid changes caused by solar input and daytime heating. Crusts will come and go depending on the extent of the overnight freeze and the weather on any given day. Good skiing is found on upper elevation north aspects, and these can be considered more "wintery" in nature for much of the coming week with more flurries forecast and cool temperatures persisting.

Régions couvertes