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The climate of the Alps is the climate, or average weather conditions over a long period of time, of the exact middle Alpine region of Europe. [ 1 ] [ 2 ] As air rises from sea level to the upper regions of the atmosphere the temperature decreases .
The Alps are split into five climatic zones, each with different vegetation. The climate, plant life, and animal life vary among the different sections or zones of the mountains. The lowest zone is the colline zone, which exists between 500 and 1,000 m (1,600 and 3,300 ft), depending on the location.
The Alps continue fairly smoothly into the following related Alpine mountain ranges: the Apennines to the southwest, the Dinarides to the southeast and the Carpathians to the northeast. In the east the Alps are bounded by the Viennese Basin and the Pannonian Basin, where east–west stretching of the crust takes place.
Image of the Swiss Alps, covered in snow during the daytime. The Alpine region of Switzerland, conventionally referred to as the Swiss Alps, [1] represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, one of its three main physiographic regions.
All the ranges in the Alpine region have high altitude, rugged terrain and a relatively cold and harsh climate. The mountains all have the same zones of vegetation, but further north the low temperature zones are found lower down. On the lower slopes there are forests and grasslands.
While smaller groups within the Alps may be easily defined by the passes on either side, defining larger units can be problematic. A traditional divide exists between the Western Alps and the Eastern Alps, which uses the Splügen Pass (Italian: Passo dello Spluga) on the Swiss-Italian border, together with the Rhine to the north and Lake Como in the south as the defining features.
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There are multiple definitions of alpine climate. In the Köppen climate classification, the alpine and mountain climates are part of group E, along with the polar climate, where no month has a mean temperature higher than 10 °C (50 °F). [1] According to the Holdridge life zone system, there are two mountain climates which prevent tree growth :