Boletín de aludes

Galena Summit & Eastern Mtns

Sawtooth Avalanche Center
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Peligro de aludes

Thu
Alta montaña
3 · Notable
Límite del bosque
2 · Moderado
Bajo el límite
2 · Moderado
Desactualizado: este boletín caducó 4 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

You're most likely to trigger avalanches where the wind has drifted or stiffened the snow on slopes facing west-north-east. As the day progresses, snowfall and wind will increase both the size and likelihood of triggering avalanches. You could trigger avalanches remotely - from gentler terrain above, below, and to the sides of steep slopes. 

The danger will increase dramatically tonight. Avoid steep slopes if you're out after dark. 

Problemas de aludes

  • Persistent Slabs

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

    What is it?  In terrain exposed to the wind, expect to find 1-2 foot thick, soft and stiff slabs perched above weak faceted snow and crusts. In more sheltered terrain, the chances of triggering smaller avalanches will rise this afternoon as a slab builds on top of weak faceted snow and thin crusts in the upper part of the snowpack.  

    Where is it?  Fortunately, this is pretty simple. You are far more likely to trigger avalanches big enough to bury you  1) where the wind has formed large drifts and slabs  and 2) on shadier aspects facing west-north-east where the snow is weakest in the upper part of the snowpack. Wind-loading should occur primarily near ridgetops and in chutes and gullies. In windier alpine areas, you may also find wind slabs lower in cirques and bowls and near prominent terrain features. The weak layer exists at all elevations, but winds will form thicker and stiffer slabs as you climb in elevation. While the snow is weakest at lower elevations, many slopes are currently lacking the slab component of the avalanche equation (weak layer + slab + steep slope). 

    How can you recognize it?  Multiple groups reported snowpack collapsing, cracking, or recent avalanches yesterday; these red flags are obvious signs of instability. Wind-loaded areas will feel stiffer under your skis or sled and are more supportable. The weak, faceted snow is fairly easy to see by digging in the snow with your hands (see photo below). You'll also find weak facets surrounding the thin crusts in the upper part of the snowpack on sunnier, SW-S-SE facing slopes.       

    How can you manage it?  Persistent slab avalanches are tricky. You could trigger them remotely (from gentler terrain above, below, and to the sides of steep slopes), and they may break wider than expected or higher on the slope above you. Avoiding areas where slabs exist above weak faceted snow or thin crusts is the conservative way to manage this problem. While today's avalanches should not be huge, it's easy to get injured in small slides when the snowcover is so thin. 

    ADDITIONAL DISCUSSION: Avalanches you trigger could "step down" to weak faceted snow buried near the ground, causing a larger avalanche. While avalanches are more likely to release in the upper part of the snowpack, we can't rule out the possibility of slides failing on the large, grey, sugary snow crystals near the ground. Read Ben's Conditions Blog entry for more information about this weak layer. 

    (11/29/2022) Several natural avalanches are visible in this photo of Eureka Peak, above the Beaver Creek drainage just west of this zone. The slope pictured faces E/NE and crown elevation ranges from 9,500-10,000'. Based on the appearance of the crowns, these slabs likely failed on the weak snow that developed during the mid-November drought. These avalanches occurred after only 6-8" of snow fell overnight on Sunday and into Monday.

Avalanche Discussion

We're not wondering if the weak faceted snow/surface hoar that developed before Thanksgiving will fail, we're wondering when it will fail.  Why is that?

  • This weak layer has terrible structure. We are impressed by how awful it looks and feels. 
  • This persistent weak layer produced natural avalanche activity after being buried by only 4-10" of snow in neighboring zones in the past week (see photo below). Even that small amount of soft new snow was enough to produce natural and triggered avalanches on slopes that were NOT heavily wind-loaded. 
  • With minimal new loading, we and other travelers are observing snowpack collapsing and long-running shooting cracks.
  • We're about to "thump it" with a big load, beginning today. 

When will it fail? Good question! The terrible structure, the unusual thin + soft slab avalanche activity, and the collapsing and long-running snowpack cracking in recent days say it won't take much to tip the stability scales. Stability could significantly worsen while you're out playing today, especially on slopes exposed to any wind. I'd be leery of steep, sheltered slopes that receive more than about 6" of new snowfall today. Looking ahead: we'll be staying out of the way while the mountains put on a show Thursday. 

The moral of the story:

  1. Avoid wind-loaded slopes, especially those facing W-N-E, where an avalanche would carry you into terrain traps or through rocks or trees.
  2. Have a conservative exit plan that is free from avalanche hazard if you're returning near or after sunset today.

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