Bollettino valanghe

South Rockies

Dec 8 – 9, 2013Avalanche Canada
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Archiviato · scaduto 13 years ago

Pericolo valanghe

Tue
Wed
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
    1–3
    Winds from the N-NE have developed wind slabs in the alpine and in open areas at treeline on SW-S aspects. These wind slabs may be easier to trigger in areas where a weak layer exists.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    1–4
    Sugary facets at or near the base of the snowpack likely represent the most worrisome persistent layer at this time. The most likely place to trigger them is on steep, convex slopes with a thin snowpack.

Confidence

Poor - Due to the number of field observations

Weather Forecast

The strong arctic high will gradually start to break down. Weak frontal waves will cross the interior regions, bringing some cloud cover and light snowfall amounts. The next significant change in the pattern should develop mid-week.Monday: Mix of sun and cloud. Alpine temperatures show a high of -18. Ridgetop winds will blow moderate from the SW. Snow amounts near 5 cm.Tuesday: Cloudy. Alpine temperatures show a high of -14. Ridgetop winds will blow light from the West. Snow amounts near 5 cm.Wednesday: Mainly cloudy. Alpine temperatures show a high of -9. Ridgetop winds will blow light from the West. Snow amounts 5-10 cm.

Avalanche Summary

No reports of avalanche activity.

Snowpack Summary

Widespread surface hoar and surface facetting continues to develop. Snowpack depths at treeline seem to vary from 80 - 120 cm. Strong ridgetop winds from the N-NE has redistributed snow onto S-SW aspects, creating reverse loaded slopes. Widespread wind effect is noticeable in the alpine and at treeline, but reports suggest wind slabs are stubborn to trigger.Below the recent storm snow down 30-40 cm sits a surface hoar/ facet/ crust interface. Snowpack testing showed easy results and some whumphing (failure of a weak layer below your feet). If you're seeing or feeling this, consider it a direct indicator of a buried weakness below.Near the base of the snowpack, I suspect you will find sugary weak facets. This layer may be stubborn to trigger under the current conditions, but if it was to happen, it would most likely be on a steep, convex slope with a thin snowpack

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