Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Up to 2 feet of snow has accumulated in the Tetons since Friday. You are most likely to trigger an avalanche on slopes steeper than 30°. Upside-down conditions exist and warming temperatures throughout the day will continue to settle the new snow into a more cohesive slab. This storm slab is sitting on a variety of surfaces including the widespread, slippery crust that formed during the warm spell last week on all aspects up to 10,000 feet. There is also a mid-storm interface down 8-10 inches in many locations that may be more prone to easy shearing. Watch for shooting cracks and feel for cohesiveness and areas of increased density, particularly in more wind exposed areas. Hand shear tests and pole probing can give you an idea of density changes and cohesiveness. Jumping on small convexities and test slopes can be a great indicator of storm slab sensitivity. Choose conservative terrain less than 30°.
Storm snow SWE has totalled over 1.5 inches in some areas. While unlikely, it is possible that with the increased weight on the January 4th interface, an avalanche triggered in the storm slab could step down to weaker layers and propagate larger than anticipated. I expect this would be most likely in steep, shady, upper elevation terrain where the crust from last week is thinner or nonexistent.
Finally, with the new snow, watch out for sluffing in steep terrain that could entrain enough snow to knock you off your feet.
(2/4/2024)
Small pockets of new snow could be cut and avalanched easily on the old snow/new snow interface around 8-12 inches deep.