Boletín de aludes

Central Sierra Nevada

Sierra Avalanche Center
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Peligro de aludes

Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
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Desactualizado: este boletín caducó 10 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

MODERATE avalanche danger exists for all elevations today. Wet loose and wind slab avalanche problems remain an ongoing concern. Precipitation intensity will be dramatically less today than yesterday and the snowpack has had time to establish drainage for rain on snow. Human triggered avalanches remain possible today. Natural avalanches are unlikely, but not impossible today in isolated areas. Exercise caution for travel in or below backcountry avalanche terrain.  

Problemas de aludes

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1

    Rain soaked surface snow below 8,500' to 9,000' will remain prone to wet loose avalanche problems today. The vast majority of wet loose avalanche activity is expected to be human triggered and occur on any aspect where wet surface snow exists. This avalanche problem will exist on slopes steeper than 35 degrees.

    Consider how terrain features below such as cliffs or terrain traps could magnify the consequences of being pushed around by a wet loose avalanche.

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2

    Above 8,500' to 9,000' where significant amounts of new snow have accumulated, wind slab avalanche problems remain an ongoing concern. Unstable wind slabs are most likely to exist near treeline and above treeline on NW-N-NE-E-SE-S aspects on slopes 35 degrees and steeper. Wind slabs could exist in isolated areas below treeline or on SW-W aspects as well due to the strength of the recent winds. Avalanche size could be fairly large at the upper elevations.

    Looks for signs of recent wind loading such as cornice features and wind pillows to help identify where problematic wind slabs are likely to exist.

Avalanche Discussion

Observations made yesterday on Andesite Ridge (Donner Summit area) revealed that a widespread cycle of wet slab avalanches had occurred from rain on recent new snow. Some avalanches appeared older than others indicating that the cycle was not limited to a short specific time window. Signs of numerous avalanches size D1 and D2 were seen on N-NE-E-SE aspects in the Donner Summit area. Significant amounts of standing and running water were noted at pass level (7,227'). Poor visibility greatly limited the ability to see signs of avalanche activity in the higher surrounding terrain.

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