Boletín de aludes

South Rockies

Nov 25 – 26, 2013Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

Wed
Thu
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
Sin grado
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Lo esencial

Check out the South Rockies Blog for thoughts on early season forecasting in this region. If you have recent observations please send them to [email protected]

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    The region has seen a lot of wind in the last week.  If an open line at and above treeline looks good enough to ski or ride the feature may be wind loaded.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–3
    Smooth alpine slopes that did not previously slide are still of concern. With very little data on the current conditions, I would treat all slopes as suspect until proven otherwise.

Confidence

Poor - Due to the number of field observations

Weather Forecast

Synopsis: The current pattern persists through the forecast period. On Wednesday a weak frontal system should clear out the inversion. No significant change in the weather for the forecast period.Tuesday: Freezing Level: Near 0 C at Valley Bottom, above freezing layer from 1500 - 3000m. Precip: No significant precip expected. Wind: Light SWWednesday: Freezing Level: 1200m Precip: No significant precip expected. Wind: Light, Variable.Thursday: Freezing Level: Valley Bottom Precip: No significant precip expected. Wind: Light, SW switching to Moderate W in the late afternoon.

Avalanche Summary

The last reported avalanche activity was during the tail end of the storm on Tuesday Nov 19th. If you see or trigger an avalanche, please send us a note at: [email protected]

Snowpack Summary

Observations from this region are EXTREMELY limited at the moment!Treeline snowpack depths in sheltered areas vary between approximately 40-80 cm. Since the snow stopped falling on Nov 19th it has been subjected to strong wind, cold temps and chinook driven warming. As a result it should be easy to find wind scoured snow, old windslabs, temperature crusts & facet formation in a single day's ride or tour.A crust or significant density change may exist around 40 cm below the surface. This has been reported to have weak faceted crystals above and below, and produces sudden "pop" results in compression tests. Below this near the base of the snowpack, an earlier crust buried in October lies close to the ground. This layer may still be of concern on isolated smooth terrain features that have not seen avalanche activity.

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