Bollettino valanghe

Purcells

Jan 5 – 6, 2016Avalanche Canada
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Archiviato · scaduto 11 years ago

Pericolo valanghe

Thu
Fri
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato

In sintesi

New snow and wind are combining to build new wind slabs above weak layers of surface hoar and facetted loose snow. Recent sun crusts may act as an easy sliding layer on southerly aspects.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Thin wind slabs may continue to develop due to forecast new snow and wind. Southeast winds may create some reverse loading in the alpine.
  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2–4
    Buried weak layers of surface hoar may be triggered by human activity. This problem is more likely in the area west of Kimberley, but may be found in shallow snowpack areas across the region.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

A weak low pressure system is slowly moving from the southern interior towards the northwest. This system is difficult to forecast for snowfall amounts. Generally there is not a lot of moisture associated with this low pressure, however some areas may receive another 5-10 cm of light dry snow overnight and Wednesday. Freezing should remain at valley bottoms for the forecast period. Winds are expected to be light easterly for the forecast period.

Avalanche Summary

No new natural avalanches reported. Some loose snow avalanches up to size 1.0 continue to be reported from steep shaded aspects in the alpine.

Snowpack Summary

Light new snow falls have buried large surface hoar on all aspects at and below treeline and on shaded aspects in the alpine. Easterly winds associated with the new snow may have disturbed surface hoar in the alpine. New snow on southerly aspects may be sitting on a sun crust and/or surface hoar, providing an easy sliding layer. The new snow should be mostly unconsolidated except where it has been re-distributed by the wind. Fresh wind slabs may be sitting on 10-20 cm of facetted snow on all but steep solar exposed aspects. In the southern Purcells, (west of Kimberley), a prominent layer of buried surface hoar has shown to be reactive to human triggers. In this part of the region, it's buried down 40 cm with a cohesive slab above it. Shallow snowpack areas and moraine features may have weak facetted snow near the ground that will require time and some warming to strengthen.

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