Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
Long lasting layers of weak snow are the name of the game this year. The character of these weak layers varies by aspect and elevation, but you can find them just about everywhere you look. The most widespread layer is a stripe of surface hoar that can be found in the lower to middle portion of the snowpack. This surface hoar has produced most of the human-triggered avalanches that have been reported to us this year. In addition, weak snow near the ground exists on many middle and upper elevation slopes.
Persistent weak layers present a complex and frustrating problem for backcountry travelers. They can continue to produce avalanches many weeks after they are buried and they provide fewer and fewer obvious signs of instability as the days without a major loading event pass. They can break wider than you might expect and may be triggered remotely, from gentle terrain adjacent to steeper slopes. Read about my thoughts on how I deal with this type of problem in my personal travels in the Forecast Discussion section found below.
Additional Discussion
I traveled through upper elevation terrain on Galena Peak yesterday to get a closer look at the recently formed wind slabs. I experienced some localized cracking in these slabs, particularly where they were sitting on stiff, icy surfaces. And, even though these slabs were posing a hazard in their own right, that was a bit of a moot point. I found that the underlying persistent slab problems described above were keeping me out of the terrain where I might have been able to trigger a wind slab.