Wind slab
- Above 2,300 m
Fresh and older wind slabs in the high Alpine regions.
Fresh and older wind slabs in the high Alpine regions.
As a consequence of new snow and a sometimes strong wind, wind slabs formed adjacent to ridgelines and in gullies and bowls. Wind slabs can be released, in particular by large loads. There is a danger of falling on the icy crust. As a consequence of the solar radiation, the likelihood of dry and wet avalanches being released will increase a little in particular on sunny slopes.
In particular adjacent to ridgelines and in gullies and bowls wind slabs formed. The surface of the snowpack will freeze to form a strong crust and will soften later than the day before. The solar radiation will give rise as the day progresses to moistening of the snowpack at low and intermediate altitudes.
Bulletin data: Arpa Piemonte (via EAWS / avalanche.report)