Boletín de aludes

South Columbia

Dec 4 – 5, 2013Avalanche 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

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    2–4
    Strong NE winds have redistributed loose surface snow into reactive wind slabs on southwest facing terrain. This is an atypical loading pattern which has the potential to catch skiers/riders by surprise.
  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    2–4
    This persistent slab will be tricky to manage as it overlies a variety of weak surfaces. A conservative and investigative approach is required for safe mountain travel.

Confidence

Fair - Due to the number of field observations

Weather Forecast

A strong Arctic air mass will continue to dominate conditions in the southern interior. Thursday: Mostly sunny, light NE alpine winds, alpine temperatures around -20CFriday/Saturday: Mostly sunny, light NE alpine winds possibly increasing on Saturday, alpine temperatures as low as -30C

Avalanche Summary

Several natural avalanches to size 2.5 were recently reported across the forecast region on all aspects.  These avalanches primarily consist of the previous storm snow or redistributed wind slabs sliding on the late-November crust/surface hoar interface. 

Snowpack Summary

Snowpack depths are typically 100-140 cm at treeline elevation. The previous storm snow (~30-60cm) overlies the late-November interface which typically consists of sun crusts on steep south facing slopes and surface hoar in sheltered areas. These weak layers are expected to be persistent and will continue to create avalanche problems in areas with enough overlying snow. The current cold temperatures will contribute to the persistence of this weak layer.  Strong NE winds after the storm have caused reverse loading and wind slab formation on SE through W aspects in wind exposed areas.  There are two layers of concern within the mid/lower snowpack but these have recently become inactive: the early November surface hoar is roughly 60cm above the ground and the October rain crust is at the base of the snowpack. While these layers have recently become inactive, residual risk of large, destructive avalanches exists, especially in areas with a thinner snowpack. The October crust can be found in the alpine on north aspects and the early November surface hoar appears to be isolated and drainage specific.

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