The fresh fallen snow in the northern regions from the beginning of this week, together with the freshly generated snowdrift
accumulations, are still prone to triggering in some places on north-facing and east-facing slopes at high altitudes more
than anywhere else. This has been confirmed by isolated avalanche triggerings from Wednesday.
During Wednesday night, a melt-freeze crust will form on the snowpack surface which in the northern and the eastern regions
will be breakable in some places. Beneath the fresh fallen snow the snowpack is thoroughly wet on south-facing slopes far
up into high alpine regions, on west-facing and east-facing slopes below approximately 3000 m, and on north-facing slopes
below approximately 2400 m.