Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 1–2
The wind slab portion of the avalanche problem is pretty simple today. Over 2’ of low density snow has fallen in favored portions of this zone. Winds are easily transporting this new snow into thick drifts. As you gain elevation, you will be more and more likely to find these slabs and they will grow in thickness and distribution. They will be most sensitive in upper elevation terrain where winds are strongest and the winds are transporting the most snow.
Yesterday, I was up high in the Smoky Mountains when the wind speeds increased. At upper elevations, the wind was quickly building slabs out of the low density snow that fell in the past two days. I found that these slabs were sensitive to my weight and I avoided avalanche terrain. As I skied back down, I found that much of my skin track had already been buried by wind drifted snow. When I returned to my sled on the valley floor, I could see that even at lower elevations the wind was moving snow.