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The continent of Europe comprises a large part of the Palearctic ecozone, with many unique biomes and ecoregions. Biogeographically, Europe is tied closely to Siberia, commonly known as the Euro-Siberian region. The European Environmental Agency (EEA) divides Europe into a total of eleven terrestrial biogeographical regions and seven regional ...
An image of the Gulf Stream's path and its related branches The average number of days per year with precipitation The average amount of sunshine yearly (hours). The climate of western Europe is strongly conditioned by the Gulf Stream, which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the United Kingdom and coastal Norway.
The challenges to habitats and species vary across Europe due to differences in climate, topography, soil conditions and so on, but the problems and solutions may be similar between neighboring countries, which may benefit from coordinating conservation efforts for sites within the same biogeographical region. [3]
Dfa climates usually occur in the high 30s and low 40s latitudes, with a qualifying average temperature in the warmest month of greater than 22 °C (72 °F). In Europe, these climates tend to be much drier than in North America. Dsa exists at higher elevations adjacent to areas with hot summer Mediterranean (Csa) climates. [10]: 231–32
The fauna of Europe is all the animals living in Europe and its surrounding seas and islands. Europe is the western part of the Palearctic realm (which in turn is part of the Holarctic ). Lying within the temperate region , (north of the equator) the wildlife is not as rich as in the hottest regions, but is nevertheless diverse due to the ...
A Köppen-Geiger climate classification map of the European Union [1] The European Union is generally characterized by a temperate climate. Most of Western Europe has an oceanic climate, in the Köppen climate classification, featuring cool to warm summers and cool winters with frequent overcast skies.
An important factor in the local climate and ecology of Central Europe is the elevation: an increase of elevation by 1,000 metres (3,300 ft) causes the average air temperature to drop by 5 °C (9 °F) and decreases the amount of water that can be held by the atmosphere by 30%.
This category covers the different Climates that exist on the Earth and other celestial bodies. See also: ... Climate of the Arctic; Climate of the European Union;