Boletín de aludes

Sea To Sky

Mar 28 – 29, 2012Avalanche Canada
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Archivado · caducó 15 years ago

Peligro de aludes

Fri
Sat
Alta montaña
4 · Fuerte
Límite del bosque
3 · Notable
Bajo el límite
3 · Notable
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Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1–4
    New windslabs are growing in lee locations over the slick melt freeze crust and spotty surface hoar. Some thin windslabs formed in unusual places from downflow winds on the weekend; these will now be disguised by the new snow.

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–6
    Cornices are very large and may become more fragile with the increased load and wind.

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    The heavy, new snow may sluff in steep terrain at lower elevations

Confidence

Fair - Forecast snowfall amounts are uncertain

Weather Forecast

Expect precip to ramp up overnight and into Thursday morning, with as much as 25cm of new snow and strong southerly winds. The freezing level should fall overnight then reach a maximum of 1200m. Friday / Saturday: Precipitation should slow down with winds turning from southerly to westerly. Freezing levels will fall as the flow turns, bringing more seasonal temperatures.

Avalanche Summary

Small windslabs (to size2.0) are forming in lee locations, and are triggering naturally and with rider traffic with limited propogation.

Snowpack Summary

Above 1700m, 30-40cm of new snow now overlies the March 26 interface. This has been accompanied by consistently moderate and at times gusty southwesterly winds forming windslabs in lee locations. Cornices are huge, and will continue to grow with this weather pattern. The 0326 interface is a crust on all aspects except true north treeline and alpine, where small surface hoar is present in sheltered places. At lower elevations, the surface snow has had less recovery and the upper snowpack is predominantly moist. Below the newest storm interface, last week's storm snow is well settled and bonded, with further strength gains deeper in the pack.

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