Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
If you are searching for drier snow at the upper elevations, you will need to assess the bonding of the new snow to the old snow surfaces. On the sunny slopes, there are slick sun crusts beneath the new snow, and even a small slide triggered in steep terrain could entrain snow as it moves down slope, resulting in a surprising large pile of debris.
On the upper elevation shady slopes, the new dense snow may not bond well to the dry, possibly faceted, snow beneath, and it will be possible to trigger sluffs or soft and medium density slab avalanches. I would also expect a few wind drifts along the higher ridge lines, mostly on the northerly facing slopes. Signs of wind drifts include cracking of the snow and looking for smooth, rounded drifts that may be denser than the snow around them.
Start with slope cuts on small test slopes to evaluate if all the new snow is bonding to the old snow surfaces, or if there are any weaknesses within the new snow. For any long running slides, the character will change from dry snow to wet snow as they move down slope through warmer snow.
In the backcountry, you will have to travel through the wet snow zone to reach the drier snow at the upper elevations. See Wet Snow Below.