Boletín de aludes

South Coast Inland

Mar 29 – 30, 2017Avalanche Canada
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Archivado · caducó 10 years ago

Peligro de aludes

Fri
Sat
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Forecast warm weather and potential extended sunny periods on Thursday and Friday will keep the avalanche danger elevated

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    New snow accumulations combined with moderate southerly winds have been building wind slabs.
  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    Recent warm and windy weather has been promoting cornice growth.

Confidence

Moderate - Timing or intensity of solar radiation is uncertain on Thursday

Weather Forecast

THURSDAY: Cloudy with sunny periods and isolated flurries / Light moderate west wind / Alpine temperature -3 / Freezing level 1500mFRIDAY: Mix of sun and cloud / Light southwest wind / Alpine temperature -2 / Freezing level 1200mSATURDAY: Flurries / Light to moderate southwest wind / Alpine temperature -1 / Freezing level 1400m

Avalanche Summary

Several thin wind slab avalanches in steep lee loaded exposed terrain were reported on Monday and Tuesday in the north of the region. One report of a cornice collapse in the south of the region on Sunday that resulted in a slab avalanche.

Snowpack Summary

Steady light snowfalls over the last week have accumulated 40-60cm of new snow in the region. Freezing levels to 2000m or higher and intermittent sun over the same time period created a variety of  thin crust layers within the upper snowpack at lower elevations and on solar aspects. A thick rain crust forming in Mid-March up to the 2100m elevation is down 50-80cm below the surface. In the north of the region, the February persistent weak layers may still be found and are down 100-140cm. They include a buried surface hoar layer as well as a crust/facet layer. In the southern parts of the region, the mid and lower snowpack are generally well settled and strong.

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