Bollettino valanghe

Cariboos

Mar 11 – 12, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

Wed
Thu
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
2 · Moderato

In sintesi

A warm and wet storm is developing. Strong winds, a heavy storm load, and rising temperatures are increasing the avalanche danger.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–6
    A weak layer of surface hoar buried down about 100-150 cm (February 12th layer) may be triggered by the new load of storm snow or by avalanches in motion.
  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–4
    New snow and wind transported snow are expected to develop a new storm slab which may be above a weak layer of surface hoar and/or a sun crust.

Confidence

Fair - Forecast snowfall amounts are uncertain on Tuesday

Weather Forecast

Overnight and Tuesday:  A warm front is forecast to move into the interior overnight bringing cloud and strong Southwest winds. Moderate snow fall amounts are expected to begin by early morning. Freezing levels are expected to rise to about 1000 metres.Wednesday:  Continued moderate precipitation overnight becoming heavy during the day combined with strong Southwest winds as the cold arctic air to the North collides with the warm front.Thursday: Unsettled weather with continued light to moderate precipitation and moderate Westerly winds.

Avalanche Summary

One natural cornice fall was reported that released size 2.0 from a Northeast aspect in the alpine.

Snowpack Summary

There is a thin layer of new snow and wind transported snow that is covering a widespread layer of surface hoar that developed during the recent clear weather. Sun crusts also developed during the clear weather on solar aspects up to about 2000 metres. Some areas had strong winds before the surface hoar was buried, so the distribution may be specific to sheltered and shaded terrain features. There is still concern for the buried weak layer of surface hoar from February 12th that is now down more than a metre in most places. The forecast new load of snow and wind may overload this deeply buried weak layer in areas that did not slide after the last storm.

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