Boletín de aludes

Kootenay Boundary

Mar 24 – 25, 2015Avalanche Canada
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Archivado · caducó 12 years ago

Peligro de aludes

Thu
Fri
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

The snow surface should freeze overnight tonight at all elevations, resulting in lower danger early in the day on Wednesday.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3
    Sunshine and daytime warming could weaken fresh wind slabs that have formed in lee and cross-loaded terrain.
  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–2
    Loose wet slides are likely on steep sun-exposed slopes during the day. 

Avalanche Summary

On Sunday and Monday a few size 1-2 storm slabs were reported from the northern part of the region. These were all from NW-NE aspects between around 2000 and 2300 m. One slide on Sunday was reported as a size 2.5 that may have been triggered by a cornice fall and appeared to release on the mid March crust.

Confidence

Fair

Weather Forecast

Wednesday: Cloudy with sunny breaks. The freezing level is near 1800 m and winds are light to moderate from the SW. Thursday: A mix of sun and cloud. The freezing level rockets up to 2500 or even 3000 m. Winds are light from the SW. Friday: A mix of sun and cloud. Remains warm with freezing levels near 3000 m. Winds remain light or moderate from the SW.

Snowpack Summary

In the past 3 days many areas received up to 20 cm of new snow above 1600 m. Fluctuating temperatures have resulted in variable snow surfaces (dry, moist, crusty) depending on aspect and elevation. Moderate W-SW winds have formed fresh wind slabs in lee and cross-loaded terrain at and above treeline. The mid March crust layer is now down 40-60cm. Recent reports suggest that the overlying snow is bonding well to the crust. At many elevations, melt-freeze cycles continue with a weak surface crust forming overnight and then breaking down during the afternoon.

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