Current situation
Let's refrain from complaining about the snow situation in non-Piedmont. After all, much is a question of attitude. Snow is fascinating and there are some particularly interesting processes to observe at the moment! Thanks to the very dry air and the strong sunlight (it may be December, but the cloudless conditions mean that some snow is still falling on south-facing slopes), the beginnings of penitential snow are slowly forming. Instead of melting in the sun, the snow sublimates when the air is sufficiently dry, so the water molecules change directly into a gaseous state. As a result, rough, jagged formations gradually form and the snow surface becomes increasingly bumpy. We are still a long way from the meter-high penitentes of the dry Andes, but this effect has been observed on a small scale on local southern slopes in recent days, provided there was any snow at all. Incidentally, several 100-metre-high penitentes of nitrogen and methane ice are suspected on the surface of Pluto!
Or, as unnamed people from the WB circle of acquaintances like to say: there is little snow, but at least it's not good.
Anyway, the weather is moving a little and the conditions for penitential snow are getting worse. The stubborn, huge Atlantic high is still in the west (or north - it reaches as far as Greenland) and is preventing any westerly weather that could bring large amounts of moisture. Instead, cold air and low pressure will push towards the Alps from the north-east. The first wave of colder air, including a few clouds and even some snowflakes in the far east, reached us yesterday.