Bollettino valanghe

Northwest Inland

Jan 21 – 22, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

Wed
Thu
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–4
    Hard and soft wind slabs may be found on many slopes, even at treeline. Although they are gaining strength, it may be possible to trigger a wind slab with the weight of a person or snowmobile.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–6
    A deeply buried facet/crust weakness exists near the base of the snowpack. This layer could be triggered by large loads such as a cornice collapse or from a thin-spot trigger point.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain for the entire period

Weather Forecast

Two frontal systems are due to affect the area, but the timing of these is uncertain.Tuesday: Moderate S wind.  Alpine temperature near -1. Light snow.Wednesday: Light to moderate SW wind.  Alpine temperature near -6.Moderate snow.Thursday: Increasing S winds. Alpine temperature near -5. Moderate snow, probably starting late in the day.

Avalanche Summary

On Friday, hard wind slabs failed naturally in the north of the region on northeast and east aspects. In isolated occurrences, these triggered full-depth avalanches that ran on basal facets. No avalanches have been reported since then.

Snowpack Summary

The current medley of snow surfaces includes hard and soft wind slabs, scoured slopes, blue ice and thin melt-freeze crusts. Surface hoar layers buried in the upper snowpack are patchy in their distribution. Recent snowpack tests gave moderate to hard, resistant results on one of these layers near Smithers. An otherwise strong mid-pack overlies a weak base layer of facets/depth hoar and the remnants of a crust. The snowpack depth is around 100 cm at treeline.

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