Abstract
The prevailing climate of west-central Europe since the retreat of the glaciers at the end of the last Ice Age (-10,000 b.p.) can be described as temperate, but there are significant differences in climate along the north-south and east-west axes. There are more than 3,500 km separating the northern and southern zones of Europe; the western coastline is influenced by the Atlantic, and the eastern zone is affected by proximity to the vast land mass of Asia. West-central Europe can therefore be described as a mosaic of climate zones that have remained distinct in spite of major climatic shifts since the end of the Pleistocene. Three major zones can be defined for the region: a marine climate zone for the western coastal region characterized by cool summers, mild winters, and significant amounts of precipitation; a Mediterranean climate zone in the south with hot, very dry summers, mild winters, and relatively sparse rainfall occurring mostly in the winter months; and a humid continental climate zone for most of central Europe with precipitation levels and summers similar to the western coast but with much colder winters.
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Arnold, B. (2001). West-Central European Early Iron Age. In: Peregrine, P.N., Ember, M. (eds) Encyclopedia of Prehistory. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1187-8_32
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DOI: https://doi.org/10.1007/978-1-4615-1187-8_32
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