Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 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.
At o'dark thirty, I'm asking myself, is it dangerous out there... will I trigger an avalanche today... can I even ride today? Yes, yes, and yes! But let's strip it down, keep it simple, and you don't need a Ouija board to figure it out. In fact, the formula is rather straight-forward-
It's dangerous if you choose steep slopes, especially those facing the north half of the compass.
The most likely place to trigger an avalanche is where a dense, strong, solid layer (slab) rests on weaker snow (Persistent Weak Layer or PWL) formed during the mid November dry-spell. That combo is found on slopes facing the north half of the compass, especially those in the wind zone at and above treeline.
But most importantly, I wanna know where I can ride and NOT trigger an avalanche. And actually that's an easy one. The powder is light, travel is easy on a very supportable base, and low angle terrain rides like a dream!
So... with no shortage of great riding in big open meadows and on low angle slopes there's plenty of opportunity to avoid pulling on the avalanches dragons tail all together.
I'm no sooth-sayer (more the Shaman type :) but I know in time our current instabilities will relax and the snow will slowly gain strength. I also know it's time to pump the brakes, continue practicing some patience, and allow the snow the adjust to the recent big storm.