Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
An early spring melt at upper elevations left our fetch bare prior to the new snow. Recent field observations confirmed that the alpine zone was bare rocks, alpine vegetation and krummholz. Wind was likely able to cross-load slopes and may have built wind slabs in isolated areas. These slabs are likely to be limited in size (D1, maybe D1.5) but a lack of field observations, particularly from the west side of the forecast area creates uncertainty in the size, distribution and sensitivity of new slabs.
(4/16/2021) This photo of Tucks was taken at 2pm after 7" of new snow had fallen. The old gray snow surface shows the degree that the new snow was scoured off of east facing terrain.