Bollettino valanghe

Purcells

Mar 29 – 30, 2014Avalanche Canada
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Archiviato · scaduto 13 years ago

Pericolo valanghe

Mon
Tue
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
3 · Marcato
Apri la mappa completa

In sintesi

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–3
    Recent accumulations have likely been blown into pockets of wind slab by generally moderate southwest winds.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–6
    There are a number of persistent layers in the mid to lower snowpack which have professional operators concerned. Possible triggers include cornice fall, thin spot triggering and/or solar warming.

Confidence

Fair - Forecast snowfall amounts are uncertain on Sunday

Weather Forecast

Sunday: Light to locally moderate snowfall. Freezing level 1600m. Light west winds.Monday: Cloudy with sunny periods and isolated flurries. Light west winds. Freezing level 1500 m.Tuesday: Mostly sunny. Freezing level 1600m. Winds west and northwest light.

Avalanche Summary

Recent reports from the central part of the region indicate a few cornice triggered avalanches to size 2.5 in the alpine on north aspects.

Snowpack Summary

Up to 50cm of new snow has fallen in the central part of the region in the last 3 days (5-10cm in the northern part of the region). This new snow is settling and likely being formed into soft wind slabs immediately lee of ridge crests.Numerous crusts can be found in the upper 60cm of the snowpack on south facing slopes. The March 15 crust/surface hoar interface is down 50-80cm. Down 90-120cm below the surface you may find surface hoar and crusts buried at the beginning of March. This interface is still touchy in some areas, particularly in the north of the region. It also continues to produce sudden planar failures in compression tests.The deeper facet/crust persistent weakness buried at the beginning of February, now down 120 - 200cm, still seems to be reactive and should not be trusted. Needless to say, any avalanche at these deeper, persistent interfaces would be large and destructive. Weak basal facets exist in many areas, but without a large load, triggering is unlikely.

Regioni coperte