Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
Field time in Tucks yesterday revealed that water was slow to percolate into the wind slabs that formed on Thursday. The 2-3cm of wet snow on the surface yesterday has likely grown much thicker due to warm temperatures overnight. As more water flows into the snow, bonds between grains will loosen and melt. This avalanche problem will not be widespread but is potentially the most destructive.