Meteocentrale Switzerland


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The average annual precipitation amounts are just above mm. In winter often a so-called inversion layer results in a large-scale low stratus cloud coverage which partly persists for several days or even weeks. Thereby the cold wind from northeast named Bise is pressed between Jura and Pre-Alps and can thus reach gale-force on the western shores of Lake Geneva. In the northwest the Jura chain edges the Midland.

With average altitudes ranging from to metres it has slightly more humid and lower temperatures in comparison with the Midland. In summer, thunderstorms are more frequent. In winter, so-called cold air pools form inside of closed valleys during windless and cloudless nights, which are responsible for especially low temperatures.

Therefore, the lowest temperature ever reached was The Pre-Alps as a transition between Midland and alpine region are among the most diversified areas in Switzerland concerning the weather. Humid air masses coming from Northern Europe dam up along the Pre-Alps and frequently cause large amounts of precipitation — significantly larger ones than in the Alps. Here again, thunderstorms become more frequent, not seldom accompanied by intensive hail.

During Foehn a warm and dry wind coming from south conditions, the temperatures are substantially higher than in the Midland and thanks to the dry air a spectacular visibility can often be enjoyed. But beware of its strength: So-called intra-alpine dry valleys as Valais Rhone Valley or Engadine are topographically shielded to the north as well as to the south. These regions not only get a lot of sun the Kleines Matterhorn above Zermatt and the Diavolezza in the Upper Engadine with to sunshine hours per year but also accommodate the driest place in Switzerland Ackersand in the Matter Valley with about mm per year.