Bollettino valanghe

Kananaskis

Jan 11 – 12, 2017Alberta Parks
Vedi sulla mappa
Archiviato · scaduto 10 years ago

Pericolo valanghe

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

In sintesi

Finally looking like its going to warm up here moving into the weekend.  Fresh windslabs that are skier triggerable are easy to find right now.  Dont get lured into big terrain, conservative choices are a must.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Recent snow and wind have created fresh wind slabs immediately below ridge crests on all aspects.  Reverse loading from the northerly winds is expected to continue.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–3
    These slabs are failing down 30-50cm at the main density change. Human triggering from a thin snowpack area is a definite possibility.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–3
    More likely to be triggered from thinner areas and step down to the November crust producing larger avalanches.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Temps are forecast to slowly warm over the next few days and winds will increase out of the NW into the 26-50km/hr range at ridgetops.  No precip in the near future.

Avalanche Summary

A few natural avalanches on N and E aspects up to sz 2 were observed over the past 24hrs.  These slides were mainly in the alpine, but in a few locations they did run down into skiable terrain.  On one slide in the murray moraines area the slab was only 20-30cm deep but was surprisingly wide (100m)

Snowpack Summary

Variable wind effect in the Alpine, with pockets of fresh wind slab immediately below ridge-crest and in crossloaded features. The Dec 18th interface is buried 40 to 70cm at Treeline and remains a concern for human triggering. The Nov crust is buried up to 100cm deep and is exhibiting facetting both above and below the crust. At lower elevations (2100m and lower in some places!) the snowpack is weak and unsupportive due to prolonged periods of facetting.

Regioni coperte