Boletín de aludes

South Coast

Jan 19 – 20, 2014Avalanche Canada
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Archivado · caducó 13 years ago

Peligro de aludes

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

Problemas de aludes

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    I suspect that the snowpack has largely adjusted to the warm temperatures. Regardless, it would be prudent to adjust travel plans to avoid sun drenched slopes in the afternoon.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    4–7
    The affect of warm alpine temps will likely diminish in the coming days, but intense direct sun could destabilize the snowpack, especially on southerly aspects.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Synopsis: A strong ridge of high pressure continues to dominate with no sign of a breakdown in sight. The freezing level continues to hover around a very un-january-like, 3000m.Monday: Freezing Level: 2500 - 3000m Precip: Nil Wind: Light, VariableTuesday: Freezing Level: 2500 - 3000m Precip: Nil Wind: Light, Variable Mod W at ridgetop.Wednesday: Freezing Level: 2000 - 2700m Precip: Nil Wind: Light, NW

Avalanche Summary

Activity on Saturday was limited to small wet point releases on solar aspects.

Snowpack Summary

Very warm alpine temperatures have created a moist snow surface. Previous winds have scoured windward slopes and sculpted sastrugi in exposed areas. Initially, the bond below the most recent storm snow was weak. However, settlement due to the warm temperatures appears to have settled the upper snowpack and it has appeared to have gained strength.There are two lower layers of note near the base of the snowpack. A facet/crust combo from late November (down approximately 100-120 cm) is still giving "sudden" results in compression tests and exists at treeline and alpine elevations. Facets and depth hoar likely still exist at the base of the snowpack, especially in areas where the snowpack was particularly shallow early on in the season. The most likely places you would find this problem is in the alpine in shallow rocky areas, and it has been most widely reported from the Duffey Lake and Chilcotin areas.

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