Recently formed wind slabs in the alpine are bonding well to the underlying layers, but there might still be isolated pockets along ridge crests which can be triggered by humans (
see the MIN report of our field team here). On higher north aspects above 2000 m new snow from early last week is gradually bonding with the dry, faceted [weak and sugary] snow underneath. In most other places surface snow is moist. Below 1800 m the entire snowpack is either moist or wet underneath a supportive melt/freeze crust.