Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Since the storm began yesterday, between 6 and 12 inches of new snow have fallen at upper elevations with minimal wind effect. This snow has fallen “right side up, " with lower-density snow falling onto higher-density snow from the start of the storm.
Storm slab avalanche size will be determined by the amount of snow in the area where you are looking to ski or ride. If you find new snow depths of a foot or more, expect avalanche size to increase accordingly. These avalanches have the potential to run far and fast on the firm bed surface of melt-freeze crusts that formed during the warm weather ahead of the storm.
Yesterday, observers noted natural avalanche activity in the Rattlesnake and were able to trigger two avalanches in the new snow. This sensitivity will continue today.
Although snow levels have dropped to valley floors, there is not enough snow at lower elevations for a continuous bed surface for avalanches.
Storm slabs are fairly straightforward to identify, and instability is short-lived. Test slopes are an excellent tool for a problem like this. Look for shooting cracks, collapsing, and fresh avalanches. Avoid convexities and areas above terrain traps like gullies, streambeds, or road cuts. Use slope angle to avoid the problem and stick to slopes under 30 degrees where avalanches are unlikely.
(2/3/2024)
A natural slab avalanche in the new snow on a wind loaded southeast aspect at 7800 ft in the Rattlesnake. It was 6-12 inches deep and around 100 feet wide.
Photo: Arden Feldman