Bollettino valanghe

South Columbia

Dec 31, 2013 – Jan 1, 2014Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 13 years ago

Pericolo valanghe

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

In sintesi

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    3–5
    A variety of buried surfaces exist and could be triggerable in the upper 100 cm of the snowpack.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    New snow is bonding poorly in the upper snowpack. Expect touchy conditions to develop with additional forecast snow and strong winds.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Thursday

Weather Forecast

Wednesday: Dry in the morning with flurries in the afternoon. Treeline temperatures around -5C. Winds NW 30-40 km/h at ridgetop.Thursday: 10-15 cm new snow expected. Freezing levels rising briefly to around 1500 m in the afternoon. Winds W 60-80 km/h at ridgetop.Friday: 2-5 cm new snow expected. Temperatures around -7C. Winds around 30 km/h from the NW.

Avalanche Summary

Two small (size 1) avalanches were reported on Monday, one on a E aspect and one on a NW aspect, triggered from ski-cutting the upper storm snow.

Snowpack Summary

Snowpack depths in this region average around 140-190 cm. 20 cm of recent storm snow has been reported to be poorly bonding to the older snow below. A weak layer consisting of surface hoar crystals, stellar crystals and/or a crust lies around 30-50 cm below the surface. At around 60-90 cm, another weak layer exists. This one was buried early December and comprises surface hoar, facetted snow, and/or a crust. It has shown variable reactivity in recent snowpack tests, but many professional operators are considering it carefully.There are two deeper layers of note. The late-November persistent weak layer consists of a sun crust on steep south facing slopes and surface hoar in sheltered areas and is now buried 70-110cm below the surface. The October deep persistent weak layer consists of a layer of facets sitting on a crust at the base of the snowpack. This layer is predominantly found on northerly aspects at treeline and in the alpine. The depth of both these layers makes directly triggering an avalanche on them unlikely (maybe a heavy load on a thin spot in steep terrain). Their presence could, however, increase the size of a potential avalanche through step-down.

Regioni coperte