Boletín de aludes

South Coast

Mar 26 – 27, 2014Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

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

Lo esencial

New snow may take some time to stabilise. Sunny periods may weaken the slab where it is sitting on a buried crust.

Problemas de aludes

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–4
    20-30 cm of new  snow has added to the recent storm slabs. The new snow may take another day to settle and bond to the old surfaces. New snow may be easily triggered during periods of strong solar radiation.
  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    3–6
    The new snow has added a new load above the deeply buried weak layers. New snow or storm slab avalanches in motion may trigger the persistent weak layers resulting in very large avalanches.

Confidence

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

Weather Forecast

Overnight and Thursday: Becoming overcast this evening with a chance of some convective flurries. Light Easterly winds overnight and during the day. Freezing levels dropping down to 600 metres overnight and rising up to 1300 metres during the day. Some chance of sunny periods in the afternoon.Friday: Overcast with snow starting in the morning and becoming heavy snow fall in the afternoon. Building Southwest winds becoming strong by the afternoon. Freezing levels rising up to about 1500 metres.Saturday: Snow and Southwest wind continuing. Freezing level rising to about 1700 metres.

Avalanche Summary

No new reports of avalanches. I suspect that there was a natural avalanche cycle in the new snow today. New snow or storm slab avalanches in motion may trigger the deeply buried persistent weak layers.

Snowpack Summary

20-30 cm of new snow overnight has added to the load of recent storm snow. The storm slab is sitting on a mix of melt-freeze crusts on solar aspects and well settled snow, surface facets, and surface hoar on shaded aspects above 1500 metres. The persistent weak layers from early March and early February continue to be a concern. The March weak layer of wind-scoured crusts, melt-freeze crusts, and/or surface hoar is reported to be down 70-80 cm. The February crust/facet/surface hoar layer is now deeply buried down 150-250 cm and may still be triggered by heavy loads like cornice falls or storm slab avalanches in motion. Long fracture propagations resulting in very large avalanches are possible with this layer. Avalanches releasing on these layers may step down to the ground during periods of strong solar radiation or warm spring rain.

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