Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 4
Here's where the rubber meets the road. The biggest clue to avalanches is... avalanches! Mark remotely triggering this piece of snow yesterday confirms all our snowpack suspicions... the fragile, sugary, and persistent weak layer (PWL) in the mid portion of our snowpack is still quite reactive to our additional weight.
The good, the bad, and the potentially ugly-
Our recent round of ultra-blower pow isn't going to wake up the avalanche dragon, but pull back the curtain and a more nefarious setup is revealed... and here's what's going on. Last weekends wind formed a dense, strong slab, but that solid layer rests on weaker snow (Persistent Weak Layer or PWL) formed during the mid November dry-spell. Now here's where it gets tricky, this setupgives us a false sense of snow stability, because it feels bomber and good to go underneath our skis, board, or sled. But the fact is, this combo isn't even letting us get onto steep slopes before weak layers fail, allowing avalanches to break remotely and well out in front of us. So yes, I'm thinking not only about the snow I'm riding in, but also the snow I'm riding on. So... any avalanche that fails near the midpack weakness (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. Yep, that pack's got a whole lotta body... baby :)