Bollettino valanghe

Jasper

Dec 12 – 13, 2015Parks Canada
Vedi sulla mappa
Archiviato · scaduto 11 years ago

Pericolo valanghe

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

In sintesi

Great skiing in Jasper right now. The Dec 3 interface down 60cm has not been reactive with this new snow, however we believe it is still touchy in isolated terrain features between 1700 - 2000m. Carefully evaluate open slopes in the trees.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2
    A touchy 15cm windslab can be found in lee areas at treeline and into the alpine. Several natural avalanches started with this slab and then stepped down to full depth releases in the alpine.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–3
    Recent snowfall has been a great addition to the snowpack, and should help set the stage for the winter. The bonding of this new snow at the Dec 3 interface down 60cm is the condition to monitor right now.

Weather Forecast

Snowfall amounts are tapering off, but a series of scattered flurries is expected to bring an additional 5cm by Saturday. Temperatures remaining cool, with daytime highs near -5C. Freezing level to remain below 1500m. Winds light and variable through to the weekend.

Snowpack Summary

70 cm of snow in the past week is settling rapidly and appears to be bonding well. The main concern is where this snow sits on the Dec3 surface hoar, most likely between 1700-2000m on sheltered North aspects. A touchy 15cm windslab can be found in lee areas at treeline. The midpack is supportive above 1700m and there is a new raincrust below 1200m.

Avalanche Summary

Numerous natural slab avalanches in the alpine up to size 3 were observed in the Columbia Icefield area as well as the lands adjacent to Marmot Basin. Several of these slides started as a storm slab, which stepped down to trigger basal weaknesses and caused large full depth avalanches. Loose dry point release were noted out of steep rocky terrain.

Confidence

Regioni coperte