Bollettino valanghe

Lizard-Flathead

Dec 9, 2017Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 9 years ago

Pericolo valanghe

Sun
Mon
Alta quota
2 · Moderato
Limite del bosco
1 · Debole
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

Avalanche danger is tightly linked to solar exposure and warming. Look to shaded aspects to find the best snow and safest riding.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    A recent wind shift from southwest to north means that wind slabs now exist on a wide range of aspects at higher elevations. Be especially cautious of reverse loaded or cross-loaded slopes that see sun exposure.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Warm, sun-exposed slopes could continue to produce wet loose avalanches either naturally or with rider triggers on Saturday - especially in steeper terrain. This problem may expand to northerly aspects as warming persists.

Confidence

Moderate -

Weather Forecast

Saturday: Mainly sunny with valley cloud due to lingering temperature inversion. Light southwest winds. Freezing level to 3500 metres with alpine temperatures around +3. Cooler at lower elevations.Sunday: Mainly cloudy. Light west winds. Freezing level to 3500 metres with alpine temperatures around +5. Cooler at lower elevations.Monday: Mainly sunny with lingering valley cloud. Light southwest winds. Freezing level to 3500 metres with alpine temperatures around +6. Cooler at lower elevations.

Avalanche Summary

Reports from Tuesday included several observations of wind slabs releasing to Size 2 in the Fernie area. These were mainly triggered with explosives but one Size 1.5 slab did release with skier traffic. Looking forward, we should see a gradually diminishing potential for wind slab releases as warm daytime temperatures and overnight cooling promote bonding in the upper snowpack. Please submit your observations to the Mountain Information Network (MIN).

Snowpack Summary

Solar and temperature crusts are expected to have formed on the surface at higher elevations over the past two days. Below the surface, recent shifting winds redistributed loose snow at higher elevations, crossloading and forming wind slabs on a wide range of aspects at treeline and above. Below this wind effect, roughly 30-60 cm of storm snow is expected to be bonding well to the underlying crust that was buried on November 26. This crust is approximately 30 cm thick and extends from 1600 m to mountain top elevations on all aspects. Below this capping crust, the snowpack is moist to ground. Average snowpack depths at treeline elevations in the region range from 80-120 cm.

Regioni coperte