Bollettino valanghe

Purcells

Mar 13 – 14, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

Fri
Sat
Alta quota
4 · Forte
Limite del bosco
4 · Forte
Sotto il limite
3 · Marcato

In sintesi

More heavy precipitation in the forecast is keeping avalanche danger high.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–7
    A significant load on the surface hoar and a sun crust buried down 60-90 cm could trigger this layer.
  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Very Likely
    Dimensione
    1–6
    Warm and wet storm has created and is going to keep developing storm slabs, new wind slabs lee of strong SW winds in the alpine and treeline, loose dry avalanches above 2000 m. and possibly wet slab and loose avalanches below that level.

Confidence

Fair - Forecast snowfall amounts are uncertain

Weather Forecast

Wednesday night and Thursday: Another wave associated with the frontal system should bring some good precipitation quantities (10-20 mm until Thursday evening) and with strong W winds easing off a bit Thursday but staying in the moderate to strong speeds. Freezing levels rising close to 2000 m.Friday: Precipitation should start tapering off as the westerly flow weakens. Temperatures and freezing level are expected to lower slightly. Winds should to remain in the moderate to strong from the W. Saturday: A little bit more precipitation is expected but no significant amounts. Light SW winds and freezing levels starting to drop significantly to reach 800 m. by the end of the period.

Avalanche Summary

2 size 2 slab avalanches were reported which would have slid on the older (pre-storm) snow surface. I suspect lots more natural avalanche activity today especially where there was significant amounts of precipitation.

Snowpack Summary

The warm storm has already added a significant load onto the snowpack (around 30 mm of water equivalent in the higher snowfall areas). Another pulse of precipitation will add weight onto the storm slab and the already moist/wet snowpack below the freezing line (around 2000 m.).  In the alpine and at treeline, the new snow will sit on a 2 cm thick suncrust on SE-S-SW facing slopes, some buried windslabs and possibly some well developed surface hoar on shaded slopes. At lower elevations, the wet precipitation will keep soaking up the snowpack possibly weakening it especially where there is a good buried sliding surface like a crust or a surface hoar layer. The surface hoar layer buried down 100 cm is still a concern and would generate a very large avalanche if triggered.

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