Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 4
Ted's pit profile from yesterday doesn't offer a whole lotta love, but I think colder temperatures will help us turn the corner... we just need to exercise a bit of patience for a minute or two.
What's the deal?
From cold to warm to warmer and even warmer yet, but now slowly cooling off, the snowpack has been yanked all over the place in the past week. Sure, we saw some natural avalanche activity with slides failing on our problem child, the persistent weak layer (PWL) of sugary, faceted snow formed by the mid winter dryspell, but the range didn't exactly come unglued. The good news is... I bet the short term pain will be long term gain for our snowpack, but before diving headfirst back into the snow I think it'll proceed with caution and consider the PWL guilty until proven otherwise.
Where does the PWL exist?
It's widespread on wind sheltered, NW-N-NE-E facing slopes near and slightly below treeline. What makes this setup so tricky is this is exactly the type of terrain we ride when it's stormy or when the avy danger is elevated. Above treeline in alpine terrain, it's distribution is more pockety.
Where and how to ride?
It's been an unusual run of weird weather, it's an atypical snowpack, and that means we need to gather some solid snow beta before comfortably getting after it and into big terrain. During your ride today, tweak small test slopes and see how they're reacting. Is your track gouging into weak, sugary snow or if you step off your machine do you sink into an unsupportable mess of damp snow. If that's case then we still need to allow some time for the snowpack to come around and gain some strength. Remember... change happens quick in the spring and I think a little patience now will deliver solid returns in the near future.