Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 4
A pit profile from the Currant Creek zone shows exactly where the weaker, sugary, persistent weak layer (PWL) exists in the mid portion of our snowpack.
Good news-
Prior to Sunday nights storm, weak, sugary faceted snow buried in the mid portion of our snowpack was just getting comfortable in its own skin, adjusting to last weeks big storm, and the lack of recent avalanche activity suggested a slow turn towards stability... good news.
Bad news-
Southerly winds cranked over the weekend, not only changed the landscape, but also adding an additional layer of strong snow to our pre-existing snowpack. Problem is... all that strong snow rests on weaker, midpack snow (our problem child, the persistent weak layer or PWL) which formed during the mid November drought.
Troubling news-
Strong snow resting on weaker snowgives us a false sense of snow stability, because it feels solid and bomber underneath our skis, board, or sled. In fact, this combo often lures us well out onto steep slopes before weak layers fail, allowing avalanches to break well above us and the whole roof crashes down. So yes, I'm thinking not only about the snow I'm riding in, but also the snow I'm riding on. Here's where the rubber hits the road and what makes things tricky right now... any avalanche that fails near the midpack PWL , is gonna break deep and wide and it's gonna be dangerous.
Unless you take your shovel out, dig down and investigate a bit, you can easily get lulled into a false sense of snow stability because the snowpack has gained a substantial amount of buoyancy and will feel strong and solid underneath or skis, board, or sled.