Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 4
Ted's image above from his travels Friday around Millcreek illustrate our problem, a persistent weak layer (PWL) buried underneath about 2 feet of snow. It's a stronger snow on weaker snow combo and that setup is causing the increase in avalanche activity. And while recent warm weather is helping our new problem child adjust, gain a little strength, and become happy in its own skin, it hasn't gone away. What this means is that the likelihood of triggering an avalanche on this layer has decreased somewhat, but we know the safest approach is to assume the PWL remains guilty until proven otherwise.
Where does this weak layer exists? The bullseye locations are basically all slopes with dry powder near and slightly below treeline today. Above treeline, the PWL is not as uniform and a little more pockety in distribution. The scary part about this situation is that this layer and it's ability to produce avalanches is variable.
How to avoid it? There are two options. (1) Ride south facing slopes where this layer doesn't exist but the riding conditions are variable. Or, (2) ride northerly facing slopes with dry powder but avoid being on or under any slope steeper than 30 degrees.
Ted and I were grabbed the video below, recapping the snow structure from our field day in upper Chalk Creek last week.