Loose Wet
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Today's intense sunshine and warm temperatures will melt the surface snow, making wet loose avalanches possible. These slides can occur naturally, without a human trigger. Where the snowpack is thin (near rocks and less than about 2 feet thick), some wet loose avalanches could gouge down to the ground. Where is this problem most likely?
- On steep, upper elevation slopes that directly face the sun: NE-E-SE aspects in the morning, S-SW aspects near noon, and SW-W-NW facing slopes later in the afternoon.
- On lower and middle elevation slopes with relatively recent, soft snow at the surface, regardless of the direction they face.
Keep an 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 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. On Friday, Chris went looking for this problem north of the highway. He found it in some of his snowpits but not in others. On an east-facing slope, he found a thin layer of facets on top of a crust, all buried beneath a 3-foot thick slab. The block did not fail during standard loading tests in his snowpack tests, but he was able to get it to break cleanly by applying some extra force.
Dealing with persistent weak layers is tricky business, particularly as they become more deeply buried. 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.