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1991; Hulme et al., 1992). Again, since the prediction of precipitation changes is intrinsically a coupled atmosphere-ocean problem, greater skill in predicting Sahel rainfall will be realized through the use of more comprehensive dynamic coupled models that include SST predictions. Each of these factors will depend on the long-term state of the climatic forcing. A condition that leads to a wet period characterized by a sequence of moderate storms may result in a higher flood potential than a period with an intense The hottest product vintage sunflower full printing low top shoesstorm. Likewise, anthropogenic changes in land use in a watershed over dec-cen time scales can significantly alter its response, and its water and sediment production potential. The interaction between anthropogenic and climatic factors at these time scales will be key to better flood-plain management. less clear is the nature of the atmospheric response to mid-latitude SST, for which theory, observations, and modeling are not yet consistent. Several mechanisms have been hypothesized to explain observed teleconnections between the tropical and extratropical latitudes, and the contributions they might make to dec-cen variability—for example, slower propagation of anomalies back to the equator via ocean processes and faster propagation from the tropics via atmospheric

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