Current situation
The current weather situation is the result of a collapsed omega blocking, from which a new, stable blocking has quickly developed. A strong area of high pressure over Scandinavia dominates the general weather situation, while low pressure lies over south-western Europe and the Mediterranean region. In between, the Alps are in an easterly to north-easterly flow with a persistent supply of cold air from Eastern Europe.
On the southern flank of the high, the trough has dripped into the Mediterranean and reactivated there. This resulted in the "high over low" situation mentioned by Lea. Such situations are predestined for persistent precipitation on the southern side of the Alps, while the north remains comparatively dry.
This was particularly evident in Piedmont: in a south to south-easterly flow, moist Mediterranean air was brought towards the western Alpine arc and converted into snowfall, sometimes heavy, by orographic uplift. North of the main Alpine ridge, on the other hand, cold, dry air dominated with intermittent clouds but hardly any precipitation.
With the gradual retreat of low pressure activity in the Mediterranean region, the transition to a calmer phase is now on the horizon - a look ahead shows how stable this will be.