Abstract
Climate has long been recognized as a major determinant of vegetation structure and composition (Woodward, 1987). Changes in climate, such as ambient temperature or the availability of light and moisture, are therefore likely to change vegetation on a relatively short time scale, such as years to decades. In fact, the connection between climate and vegetation has been considered so close that knowledge of past vegetation composition, derived from pollen, macrofossils, or other sources, could be used to reconstruct historical climatic patterns by analysis of the correlation between the presence of certain species and the climatic conditions. The key concepts that were developed for such paleoecological reconstruction have provided valuable contributions to the more recent development of predictive modeling of climate-vegetation interactions (see Huntley, Chapter 15).
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Cramer, W. (1997). Modeling the Possible Impact of Climate Change on Broad-Scale Vegetation Structure: Examples from Northern Europe. In: Oechel, W.C., et al. Global Change and Arctic Terrestrial Ecosystems. Ecological Studies, vol 124. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-2240-8_17
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