Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 4
The situation is very simple - there is a persistent weak layer (PWL) of old, faceted snow near the ground with 3-10 feet of snow on top of it. This layer has been fracturing and producing large and destructive avalanches. Winds increased from the south and have likely been loading the slopes where this PWL exists. The likelihood of triggering these massive avalanches has gone down just a little in recent days, but the size and destructive potential of these slides hasn't changed.
This layer exists on west, north, and east-facing slopes where old snow lingered and weakened in November and was buried by December snowfall. It doesn't exist on south-facing slopes because it melted away in November, and December snowfall landed on bare ground on those slopes.
Over the last week, snowfall containing up to 8 inches of water has been added to the snowpack. We focus on water amounts because that tells us how much weight is added to the snowpack. For a slope the size of a football field, snow with 8 inches of water weighs 2,800,000 pounds. Imagine that amount of snow crashing downhill.
Video from the Firewater Avalanche off of Little Water Peak in Big Cottonwood Canyon, of the central Wasatch.
How will we know when this avalanche problem heals? That's a tough question to answer, and we mainly have to let the snowpack answer it. For now, avalanches are still happening and that's all I need to know. As we look into the future, it will heal, but I can't tell you when. We will be monitoring the snowpack and avalanche activity and keep you updated.