Bollettino valanghe

Cariboos

Dec 14 – 15, 2024Avalanche Canada
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Archiviato · scaduto 2 years ago

Pericolo valanghe

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

In sintesi

Areas that receive new snow will develop small windslabs in alpine and treeline elevations.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–1.5

    New slabs may develop where new snow has been deposited by wind. Older slabs are most likely to be triggered in sheltered lee features in the lower alpine where pockets of deeper snow have been deposited over a layer of surface hoar.

Confidence

Moderate

Avalanche Summary

No new avalanches reported since Sunday. Incoming precipitation and wind will create small windslabs in alpine and treeline elevations.

Observations remain limited in this region. If you head into the backcountry, please consider sharing your observations to the Mountain Information Network (MIN)!n the alpine and treeline elevations.

Snowpack Summary

New snow will likely fall on surface hoar in sheltered locations and surface facets. 10 to 30 cm of old snow overlies a hard melt-freeze crust up to 1600 m and isolated pockets of surface hoar crystals in wind-sheltered openings at treeline and above.

There are currently no deeper layers of concern.

Weather Summary

Friday night

Cloudy with snow, 0 to 5 cm. 20 to 40 km/h south ridgetop wind. Treeline temperature -6 °C.

Saturday

Cloudy with snow, 0 to 5 cm. 40 to 60 km/h south ridgetop wind. Treeline temperature -7 °C.

Sunday

Mostly cloudy with snow, 0 to 2 cm. 20 to 40 km/h southwest ridgetop wind. Treeline temperature -6 °C.

Monday

Scattered cloud. 20 to 30 km/h southeast ridgetop wind. Treeline temperature -8 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Investigate the bond of the recent snow before committing to your line.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.

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