Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Continued snowfall Sunday night and Monday will increase our storm totals and create the potential for additional weak interfaces. Springtime temperature swings and gusty winds could also create problematic layers within the recent storm snow. To this point, most of the storm snow has been fairly low-density but these environmental factors could change that. Take the time to look at all of the snow over the 4/8 crust to determine if an upside-down snowpack has developed (where heavy snow exists over lighter, weaker snow). In addition to digging, you can use small test slopes to check how the snow is reacting to your weight. Visual clues like cracking of the surface or blocks of snow failing in upslope tests while you travel can help key you into the snow’s slab potential. If you find that slabs exist or the snow is failing easily during your tests, avoid slopes over 35 degrees where triggering an avalanche is more likely.
(4/10/2022) Widespread D1 storm slabs on convex features failed naturally during a period of high precipitation rates on the morning of 4/10. Photo: Andy Harrington