Bulletin d’avalanche

Galena Summit & Eastern Mtns

Sawtooth Avalanche Center
Voir sur la carte

Danger d’avalanche

Thu
Alpin
2 · Modéré
Limite forestière
1 · Faible
Sous la limite
1 · Faible
Périmé — ce bulletin a expiré 6 years ago. Vous consultez des conditions passées, pas le bulletin en cours.

Points saillants

Expect to find isolated wind-drifts near ridgelines in alpine and upper elevation terrain. Additional snowfall today could increase the size and chances of triggering slab avalanches, especially in the White Cloud Mtns where more snow has fallen in recent days. Periods of muted sunshine could cause wet loose snow avalanches on very steep slopes.

If you are traveling in the Pioneer Mountains, refer to the forecast for the Soldier & Wood River Valley Mtns.

Problèmes avalancheux

  • Wind Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Possible
    Taille
    1

    Yesterday, Ben found the light snowfall and moderate winds built thin, fresh wind slabs in exposed alpine terrain. They were not widespread, but they were there. With continued light snowfall and some wind in the forecast today, the slabs will probably continue to grow. 

    The wind slabs are most likely to fail on instabilities within the new snow and at the old/new snow interface, producing relatively small avalanches unlikely to bury people. But, the possibility of triggering a larger slide on faceted layers buried 1-2 feet deep is gradually increasing. The faceted snow—recognizable as or near a dirty stripe in the snowpack (view Observation)—is most commonly found on NW-N-NE aspects at middle and upper elevations. These near-surface facets buried by March storms have produced natural avalanches, cracking, collapsing, and unstable snowpack test scores in several forecast zones. 

    No matter the size of the slide, managing travel in wind-loaded terrain is straightforward; avoid slopes where you see or feel obviously wind-affected snow to reduce the chances of triggering avalanches. Look for signs of wind drifted snow such as pillows and dune-like drifts. A rippled surface texture is another good sign that the wind has been at work. If the snow depth rapidly increases, or you move from soft, powdery snow into thicker, denser snow, you are probably pushing into a wind drift. Cracks shooting out from your skis or board are a clear indication that you've found a sensitive drift. 

    ADDITIONAL DISCUSSIONEven short periods of direct or muted sunshine today could cause natural loose snow avalanches as well as increase the chances of triggering them. At upper elevations, you may see small "dribbles" involving only the new snow from the past couple of days. As you move downhill from the alpine, you could see slides that gouge down in thin snowpacks less than about 2 feet deep. Any triggered or natural wet slides should not be huge, but they could pack a punch if they are starting hundreds of feet above you. Also, they could be large enough to carry you places you don't want to be. Pay attention to what's above you if you're traveling in complex terrain. 

    If you are traveling in the Pioneer Mountains, refer to the forecast for the Soldier & Wood River Valley Mtns to read about the persistent slab problem you may encounter.

Avalanche Discussion

In all aspects of life, we sort the world into boxes to help us understand and communicate about the reality we encounter.  As avalanche forecasters, we use boxes known as avalanche problems to help describe the type of unstable snow that you might encounter in the backcountry. Different problems form in different areas and require different management strategies in order to avoid the hazard they pose. The avalanche danger is MODERATE in all of our zones today, but the avalanche problems and the hazard mitigation strategies are very different. 

In our northern areas, we are primarily dealing with a WIND SLAB problem right now. Avoiding the danger posed by a wind slab is relatively simple. (Notice the word "relatively" in there, we didn't just throw that in for fun. The backcountry environment is an incredibly complex one and we are well served to give it the respect it demands.) We can avoid wind slabs by avoiding terrain that is affected by the wind. No wind, no wind slab. If we want to cut things a bit closer, we can travel in terrain that is exposed to the wind, but where the wind has removed snow (scouring) instead of adding snow (loading). If we choose to cut our margins even closer, we can travel in terrain where the wind has been loading slopes with slabs and attempt to assess the stability of the wind slabs. Being able to do this successfully requires a great amount of experience and opens you up to high consequences if your assessment goes awry. 

In these same areas, even indirect sunshine may create WET LOOSE and DRY LOOSE avalanche problems today. The 8-12 inches of recent snowfall sits above a variety of crusts and other surfaces. It will not take much sunlight or heat to increase the cohesion in the new snow and make loose snow avalanches possible on very steep slopes. If the snow is getting "heavy", you could trigger small slides that have enough mass to push you around. A potentially bigger issue is natural slides striking you from above; loose snow avalanche problems can develop rapidly, so you need to move quickly and pay attention if you are traveling on or below steep avalanche paths. 

In the southeastern portion of our advisory area, we are currently dealing with a PERSISTENT SLAB problem. Persistent slabs are an entirely different beast to deal with than wind slabs. They form when weak, long-lived (hence "persistent") layers of snow are buried. As you just read, there are several options available when it comes to managing a wind slab problem. In contrast, a persistent slab problem presents a problem with few management strategies. Most of the time, the only real option you have is to avoid the terrain where the problem exists. We've spent many, many days in the backcountry, digging hundreds of snowpits and assessing snowpack stability. But even though the danger is "only" moderate in the Soldier and Wood River Valey zone right now, there are many slopes we wouldn't consider skiing or riding.  

Still with us here? When things are simple, the types of avalanche problems that you encounter in the backcountry feat neatly into the avalanche boxes. However, if you're old enough to be reading and understanding an avalanche forecast you probably know that the world we live in is rarely simple. The month of March has been dominated by alternating periods of snowfall and clear weather. Between storms, weak layers of snow formed at the snow surface and were subsequently buried by the next round of snowfall. In areas where wind slabs have formed on top of these weak layers, the wind slabs are adding additional stress to the weak snow underneath.

Are you facing a wind slab or persistent slab problem? We suspect you all have some extra free time today. Your challenge: spend some time thinking about what type of problem you might think of this as and how you might manage it. Call your favorite backcountry partner and ask them what they think. Today is a great day to open up your brain and learn something new. The backcountry environment always challenges us and provides us with endless opportunities to learn something new. Clear your brain of your preconceived notions and make an effort to look at this idea with fresh eyes. It is worth the time and effort. 

 

Régions couvertes