Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Weak layers of snow are buried 1.5-3 feet deep in this zone. In our other forecast areas, human-triggered avalanches were failing on this weak interface even before the new snow fell earlier this week (photo, photo). In the days since the storm, skiers and riders have triggered multiple slides that failed on this snow. On Thursday, Chris investigated an avalanche near Galena Summit that was remotely triggered by skiers from flatter terrain above. I'd recommend taking the time to watch the video he made, available at right/above.
The culprit weak layers in all of these slides have been sugary facets that developed in March during clear and cold weather between storms. The distribution and sensitivity of these layers are somewhat irregular. They have proven to be reactive on some slopes and unreactive on others. You are most likely to find them on slopes that face E-NE-N-NW. On these aspects, it's best to assume these layers exist and choose lower angled terrain not threatened by steeper slopes above. These slabs are more likely to be reactive in areas where the wind has stiffened the snow surface and added more weight (see wind slab problem described below), but they are possible in sheltered terrain as well.
Dealing with persistent weak layers is tricky business. Snowpack test results can be difficult to interpret and obvious signs of instability are often absent. The first clear sign of an unstable snowpack may occur when you trigger a large avalanche.
ADDITIONAL DISCUSSIONThe days since the recent storm have been much colder than average. Last night's temperatures were the warmest we've seen in a week. If the sun comes out for longer than expected today we may see some wet snow issues develop. Keep an eye on the condition of the snow surface. If it starts to get wet or you are seeing wet balls of snow forming and rolling downhill it is time to think about moving to an area where the snow surface is colder and drier.