Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 4
Mark describes our snowpack setup in the viddy above
Throughout the Uinta Mountains, there is a slab 2'-5' thick resting on a persistent weak layer (PWL) of facets about a foot above the ground.... think strong snow on weak snow. The PWL exists on most slopes except those facing due south and southwest.
Avalanche conditions remain deceptively tricky and here's why-
First- it's low probability/high consequence. What we know is that if we do trigger a slide, it can break 2-5 feet deep and hundreds or even thousands of feet wide and it'll be unsurvivable. Unfortunately, we don't know the exact probability of triggering an avalanche on this weak layer but it has decreased somewhat since the big Valentines storm.
Second- with such a supportable slab on top of this weak layer, a slope may have many sets of tracks on it and still slide if someone hits a thin spot in the snowpack. You can guess where thin spots exist, but you never really know because they can be near a rock or bush hidden under the snow, like in the image above.
What to do? Unfortunately it's just a season with a dangerous snowpack. There's no way around that fact, and the key to longevity is avoiding all big, open slopes steeper than 30 degrees. Slopes above treeline, especially those with recent deposits of wind drifted snow are most dangerous. Triggering a slide on slopes near treeline remains possible.