Boletín de aludes

Central Sierra Nevada

Sierra Avalanche Center
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Peligro de aludes

Fri
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
Desactualizado: este boletín caducó 5 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

Sluffs of wet loose snow will become possible on steep slopes as soon as today's sunny warm weather melts through last night's weak refreeze. Some of these could entrain enough wet snow to cause problems for backcountry travelers especially on long steep slopes or in areas with terrain traps. The avalanche danger is MODERATE today.

Problemas de aludes

  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2

    Even though temperatures remained above freezing in many places last night, the snowpack should have radiated enough heat into the clear skies for at least a thin refreeze. Today's intense sunshine and warm weather should melt through this refreeze quickly. On steep slopes, the wet loose snow that forms on the surface could slide downhill gathering more wet snow as it moves. These wet loose avalanches may start small (D1) but could end up entraining enough wet snow to cause problems (D2) on longer slopes. Terrain traps like cliffs, gullies, creekbeds, etc could make the smaller wet loose avalanches have larger consequences. The most sun-exposed E-SE-S-SW-W aspects will be the most prone to wet snow instabilities, but the high sun angles and warm temperatures could allow wet snow to form on some of the NW-N-NE aspects as well.

    Snow conditions will change from supportable to wet loose quickly today. Signs that wet loose avalanches may be possible include things like rollerballs, pinwheels, wet sticky snow, or ankle-deep wet snow. Recreating before the snow becomes unsupportable or using terrain less steep than 30 to 35 degrees without steeper slopes above can help minimize exposure to potential wet snow instabilities.

     

Avalanche Discussion

* Spring melt-freeze conditions exist on most SE-S-SW aspects. The snow surface on these slopes has been softening as the day warms up with a thick layer of wet unconsolidated snow forming by the afternoon. Most of the lower and middle elevation E and W aspects also have transitioned into spring melt-freeze conditions.   

* Upper elevation E and W aspects and most NW-N-NE aspects at all elevations still remain in between winter-like snow and spring melt-freeze conditions with a surface crust over colder dryer snow.  

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