Abstract
The mediterranean-type climate of Australia, with wet winter periods alternating with dry summer periods, is confined to the south-west corner of Western Australia, the southern portion of South Australia, and the western half of Victoria. To the north it grades into the semi-arid zone of the interior of Australia; in the east, it merges with areas receiving increasing amounts of summer rainfall. Within this zone, annual precipitation varies from 250 to 1,500 mm with 5–15% of this precipitation falling during the summer months, December to February. This small incidence of summer rainfall appears to have enabled certain growth patterns atypical of most mediterranean regions of the world to persist in the southern Australian vegetation.
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Specht, R.L. (1973). Structure and Functional Response of Ecosystems in the Mediterranean Climate of Australia. In: di Castri, F., Mooney, H.A. (eds) Mediterranean Type Ecosystems. Ecological Studies, vol 7. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65520-3_8
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DOI: https://doi.org/10.1007/978-3-642-65520-3_8
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