Loose Wet
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Very Likely
- Taille
- 2
Yesterday I observed dozens of wet loose avalanches from the southern Sawtooths to Galena Pass and on into the Wood River Valley. For the most part, these avalanches involved thin layers of wet snow near the surface. With intense sunshine and even warmer temperatures today and tomorrow I expect wet avalanche activity to continue. The size and destructive potential of these slides may increase as meltwater pushes deeper into the snowpack.
This problem is most likely:
- On steep upper elevation slopes that directly face the sun
- On slopes sheltered from the wind
- On lower and middle elevation slopes regardless of the direction they face.
Keep a close eye on the condition of the snow surface while you're traveling. When it gets wet or when you see wet snow rolling downhill, it is time to move to gentle terrain or slopes where the snow surface is colder and drier. Wet loose instabilities can develop rapidly; think minutes rather than hours. Minimize the time you spend below all large, steep slopes in the heat of the day especially those that directly face the sun.
ADDITIONAL DISCUSSION: Weak layers of snow buried 2-3 feet deep have proven to be less reactive in this zone than in neighboring areas. That said, weird avalanches tend to happen during the first major, extended warmup of the season. Dealing with persistent weak layers is tricky. Snowpack test results become more difficult to interpret and obvious signs of instability are absent. The first clear sign of an unstable snowpack may occur when you trigger a large avalanche. These types of slides can be triggered remotely—from a distance above, below, or to the side of a steeper slope—or by smaller loose snow avalanches or cornice fall coming from above.