Abstract
The mediterranean regions of the world are defined by the distinctive annual climatic sequence in which a hot, dry summer alternates with a cool to cold, humid period lasting for a period of 5–10 months from autumn through winter to spring. This characteristic climate is found on all continents.
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Specht, R.L., Moll, E.J. (1983). Mediterranean-Type Heathlands and Sclerophyllous Shrublands of the World: An Overview. In: Kruger, F.J., Mitchell, D.T., Jarvis, J.U.M. (eds) Mediterranean-Type Ecosystems. Ecological Studies, vol 43. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-68935-2_2
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DOI: https://doi.org/10.1007/978-3-642-68935-2_2
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