Bollettino valanghe

South Columbia

Dec 22 – 23, 2015Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 11 years ago

Pericolo valanghe

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

In sintesi

Low Danger does not mean No Danger. Make observations continually as you travel.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Low-density powder may be hiding wind slabs which formed during stormy weather on the weekend. They may have gained considerable strength, but I'd remain cautious on high-elevation lee slopes. Loose dry avalanches are also possible in steep terrain.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely
    Dimensione
    2–4
    A layer of buried surface hoar can be found between 1400m and 1800m. Although this layer has become unlikely to trigger, I'd remain cautious on steep roles in cut-blocks and open glades below treeline.

Avalanche Summary

Evidence of a natural cycle of soft wind slab avalanches in the size 1-2 range was observed on Monday. The avalanches occurred in response to new snow and wind over the weekend.

Confidence

High

Weather Forecast

A benign yet cool weather pattern has set up and will continue for the forecast period. For each day, expect a mix of sun and cloud with isolated flurries. Ridgetop winds are expected to remain light while alpine temperatures should remain between -12 and -16.

Snowpack Summary

10-40cm of low-density snow overlies soft wind slabs which formed last weekend. The few observations we've had suggest a good bond within the storm layers in the upper snowpack. I'd still remain cautious in upper elevation lee terrain where buried wind slabs may still be sensitive to human triggering. Between 80 and 130cm below the surface you'll likely find a weak layer of well-developed surface hoar which was buried in early December. This layer is most widespread and reactive at lower elevations (between 1100m and 1800m.) Snow pit tests suggest that human triggering of this interface has become less likely. That said, if it does fail the overlying slab is stiff enough to propagate over a wide distance. Below this layer, the snowpack is thought to be generally strong and well-settled.

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