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The Alps contain a number of different kinds of climate zones, by elevation. These zones can be described by the Köppen climate classification, and also correspond to the biotic zones of the Alps. [3] Up to approximately 1,050 metres (3,440 ft) of elevation, the climate is classified as oceanic or Cfb under the Köppen system. [3]
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.
Alpine climate is the typical climate for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate . Definition
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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They might find there's no escape. Rising temperatures in European mountain ranges are increasingly making for an unpredictable ski season, and might hurt wealthy buyers' investments.
A number of locations around the Earth have alpine climate. The climate of some of these locations is described, below. For tropical oceanic locations, such as the summit of Mauna Loa, elev. 13,679 ft (4,169 m), the temperature is roughly constant throughout the year: