Bollettino valanghe

Northwest Coastal

Nov 28 – 29, 2014Avalanche Canada
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Archiviato · scaduto 12 years ago

Pericolo valanghe

Sun
Mon
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
Senza grado

In sintesi

Cold, dry, and windy conditions persist under an Arctic ridge of high pressure.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    Watch for hard and dense wind slabs in exposed lee terrain and cross-loaded features. Triggering is more likely in steep and unsupported terrain (convex shaped, above cliffs). 

Confidence

Fair - Due to the number of field observations

Weather Forecast

A push of Arctic air from the north is bringing dry, cold and windy conditions to the northwest. Valley bottom temperatures will hover around -10 to -15. We should continue to see moderate or strong outflow winds (from the E-NE) in coastal valleys and inlets. On Sunday we could see increasing cloud and light snowfall as a system moves in from the northwest. This could also increase temperatures by a few degrees, but it will remain cool.

Avalanche Summary

A few small explosive triggered wind slab avalanches were reported north of Stewart this week. These slides were from northerly aspects near treeline and were up to 40 cm deep. We have had no reports from popular recreational spots in the region. Let us know what you are seeing at [email protected].

Snowpack Summary

As we begin our forecasting season, we are working with limited information from the field. Early reports suggest there's enough snow for avalanches at alpine and some treeline elevations. Recent snow has likely been redistributed by gusty and variable winds forming dense or hard wind slabs on lee slopes and stripping windward slopes bare. This snow may overlie a weak old snow surface (surface hoar, facets and/or a crust) which developed during November's dry spell. Check the bond of the snowpack at this level and take a cautious approach as new snow builds deeper above this layer.

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