Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
A persistent weak layer of loose, sugary faceted snow exists on W-N-E aspects beneath a slab that is 2' -3' thick. This problem is most pronounced on slopes facing NW-N-NE-E near treeline and below and the weak layer is easy to locate with your shovel. At the middle and lower elevation bands, backcountry observers continue to report failures in stability tests, collapsing, and shooting cracks. Above treeline the weak layer distribution is much more variable and it is hard to track. Attempting to outsmart this avalanche problem in the alpine is a dangerous proposition. By mid March skiers and riders in the La Sals start to think about big objectives and skiing the high peaks, but now is not the time. There is a reason we call this type of weak layer persistent, and patience is the name of the game for now. Low angle slopes remain your best bet for skiing today.
Read Eric Trenbeath's great observation from Sunday for more insight on this buried PWL.
This image illustrates the snow pack history from when it quit snowing on December 31, through now (Eric Trenbeath). To see how the snow nerds record this information, scroll down to additional information.