Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–1.5
Wind-affected terrain exists in wide swaths of the zone, but a lack of recent avalanche activity suggests that most slabs may be stubborn to trigger. A fresh round of wind transport late Wednesday night and early Thursday will maintain or build the danger slightly. Watch for signs of active snow transport to identify wind-loaded areas where you are most likely to trigger an avalanche. Cracking surfaces or hollow-feeling snow layers should put you on alert. If you encounter wind-affected snow, try assessing it with simple hand shears. If the new snow slides easily off the underlying surfaces, or you can get shooting cracks on small test slopes, it is probably time to move to lower angle terrain.
Easterly winds Monday and Tuesday have transported snow onto westerly aspects. We're uncertain how much these winds affected the majority of the East Central zone. You'll have to do some detective work to identify clues. Cornices form with the prevailing wind direction, and wind slabs from Easterly winds may form on the opposite side of the ridge with sharper cornice lips. Elevated danger may linger in the Wenatchee Mountains where strong to extreme NE winds blew low-density snow onto atypical aspects through Tuesday night. In these areas, the strong winds might have dragged wind slabs down into the NTL or even possibly exposed BTL locations. Shallow snowpacks in these areas increase your risk for trauma.
(2/23/2022)
Cracking in skin track SE at 6800ft. Fortune Creek Drainage.
Photo: Matt Primomo