Bollettino valanghe

Kananaskis

Mar 14 – 15, 2013Alberta Parks
Vedi sulla mappa
Archiviato · scaduto 14 years ago

Pericolo valanghe

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

In sintesi

Another warm storm system has added another layer of snow that is readily available for slab development. Anticipate changing conditions and be prepared for a variety of traveling conditions. Stepping down is a possibility as well.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–5
    Soft slabs and hard slabs are widespread in alpine and treeline areas. Natural avalanche activity has significantly reduced, but skier-triggering is possible in steep, convex and/or unsupported terrain.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    Alpine ridges

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–5
    New storm slabs are developing along ridgetops at treeline and above.  A combination of above freezing temperatures, moist snow and rainfall up to 2100m will result in rapid slab formation.

Confidence

Good

Weather Forecast

Temps are expected to cool off in the alpine by 5 degrees but remain around 0 for TL elevations(1500m). No precip is expected and winds are still forecasted to be strong to extreme. Another round of precip is expected to arrive Sunday. How this interacts with the existing snow will remain to be seen.

Avalanche Summary

No avalanches noted today, observations very limited due to poor vis. Bombing runs in neighboring areas triggered one notable Sz3 slab (E asp, 2300m). Cornices were reportedly very large as well.

Snowpack Summary

Inversion conditions today led to moist snow starting at 2000m. Rain crust on surface below that. Limited visibility today, but storm slabs from the ongoing wind event are certain at TL & ALP elevations. These slabs will remain reactive to human triggering in steep terrain at all elevations until the temperatures cool. The warm nature of the storm will promote slab development and cornice growth.

Regioni coperte