Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Recall that last week as we transitioned from rain to snow the storm came in with strong winds. Those winds formed dense windslabs at higher elevations and exposed ridgetops. In our outing yesterday to the Cabinets we found the windslabs still present but not as touchy. The milder weather has allowed the slabs to bond with the underlying snow. Leeward slabs tend to be thicker than windward slabs. The depth of snow over the Christmas crust varied from 1-2 feet. We did not see any natural avalanches of windslab over the crust. We did reveal some moderate shears of the new snow over the Christmas crust but in most cases it seems that the snow bonded to the crust.