As a result of fresh snow and shifting winds, snowdrift accumulations which are prone to triggering are being generated in
all aspects. They will increase in size and frequency during the course of the day. In the major areas of precipitation, the
snowdrift accumulations will be large sized. In the central Valais and from northern Grisons into the Lower Engadine, where
the least amount of snowfall is anticipated, they will remain small-to-medium sized.
In the more deeply embedded layers inside the snowpack in all regions, hardly any avalanche triggerings are to be expected.