Boletín de aludes

Cariboos

Mar 12 – 13, 2013Avalanche Canada
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Archivado · caducó 14 years ago

Peligro de aludes

Thu
Fri
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
3 · Notable
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Lo esencial

Warm, wet, and windy! The storm will cause High avalanche danger for the next few days.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    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 montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    2–5
    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. Warm temperatures and rapid loading may promote long fracture propagations resulting in large avalanches.

Confidence

Fair - Forecast snowfall amounts are uncertain on Wednesday

Weather Forecast

Overnight and Wednesday: A strong Westerly flow will continue to bring moderate to heavy precipitation and strong West-Southwest winds overnight and during the day. Freezing level rising to 1600 metres.Thursday:Continued moderate to heavy precipitation and strong Southwest winds. Freezing level at 1600 metres.Friday: The precipitation is expected to taper off as the Westerly flow weakens.

Avalanche Summary

Some thin wind slab avalanches were reported from Monday. I suspect that poor visibility and travel conditions will limit observations from Tuesday.

Snowpack Summary

A new storm slab is developing due to strong Southwest winds, new snow, and warming temperatures. The new storm snow has buried 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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