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- W1659363039 abstract "Mediterranean environments are often characterized by a double stress: summer drought and winter cold (Mitrakos 1980; Miller 1981; Terradas and Save 1992). Summer drought results from the coincidence of low summer precipitation with high temperature, high irradiance, and high water vapour pressure deficit (Di Castri and Mooney 1973); it has been traditionally recognized as the main climate constraint characterizing Mediterranean-type ecosystems. However, some degree of stress can be also due to winter cold, which may be determinant in montane and/or continental sites. This is reflected in the seasonal patterns of plant activity. Photosynthetic activity is typically relatively high in spring, decreases strongly in summer due to drought (Oechel et al. 1981, Tenhunen et al. 1990), increases again after the first autumn rains, and decreases or ceases during the winter months. Plant growth and leaf transpiration may follow similar patterns." @default.
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- W1659363039 date "1999-01-01" @default.
- W1659363039 modified "2023-10-04" @default.
- W1659363039 title "Gas Exchange and Water Relations" @default.
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- W1659363039 doi "https://doi.org/10.1007/978-3-642-58618-7_10" @default.
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