The weather-determining low-pressure area over the North Atlantic will spread southward, consequently the large-scale current over Central Europe will shift south-west to south for longer. Unseasonally mild air masses will reach us from the Mediterranean region throughout the upcoming days. The main Alpine ridge will be affected by barrier affects affected by cloudy air masses. North thereof a partly stormy south foehn will blow in the mountains, which will produce further increasing temperatures. The southerly barrier effects at the Alpine divide will be rather weak until Thursday, however, this will change afterwards. On Friday and throughout next weekend, the southerly barrier effects will increase and with the end of the foehn wind precipitation will reach the northern edge of the Alps. The temperatures will decrease and the snow line will sink below 1,500 m above sea level.

Unchangeable foehny Unchangeable mild