Bollettino valanghe

Purcells

Dec 4, 2018Avalanche Canada
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Archiviato · scaduto 8 years ago

Pericolo valanghe

Wed
Thu
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

Wind slabs may be more susceptible to human triggers where they sit above a buried weak layer. Field observations are limited, so it is critical to supplement this forecast with your own observations.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Wind slabs are most likely found on leeward slopes. They will likely be more reactive where they sit above a weak feathery surface hoar layer and/or a sun crust.
  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    1–3
    A combination of crust and faceted (sugary) snow exists at the base of the snowpack in the alpine. This layer could produce avalanches on steep, smooth slopes in the alpine.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

MONDAY NIGHT - Cloudy with clear periods / light northwest winds / alpine temperatures near -12TUESDAY - A mix of sun and cloud / light west to northwest winds / alpine temperatures near -10WEDNESDAY - A mix of sun and cloud / light northerly winds / alpine high temperatures near -10, low temperatures near -15THURSDAY - Sunny with cloudy periods / alpine high temperatures near -6, low temperatures near -10

Avalanche Summary

No new avalanches have been reported in the region, however field observations are very limited. If you have been in the backcountry, please submit your observations to the Mountain Information Network.

Snowpack Summary

The early season snowpack is highly variable in the Purcells. Approximately 20 cm of snow fell last week which may have been blown into wind slabs on exposed northerly and northeasterly slopes. There are two layers of surface hoar (weak feathery crystals) being reported in the top 35-40cm. The surface hoar is most prominent at treeline, but it may be found in sheltered alpine areas. Both of these layers may be associated with a sun crust on south aspects in some areas.In shallow snowpack areas, the bottom half of the snowpack is reportedly weak and "hollow" feeling on shady aspects due to sugary, faceted snow.A prominent feature of the snowpack is a combination of a crust and faceted (sugary) snow found at or near the base of the snowpack.

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