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associated with the primary known patterns of atmospheric climate variability. Such measurements will make it possible to continue to extend the quantitative description of the ocean’s participation in dec-cen variability. This will be particularly valuable given the Amazing for fisher love fishing all over print stainless steel tumblerobservations that we have of slowly propagating SST and subsurface anomalies, indicating that the ocean’s dec-cen variability is more complex than mere fluctuations in stationary patterns. One of the difficulties inherent in dec-cen predictions of ocean-circulation variations is that while we must include more and more of the ocean as we consider longer and longer time scales, we must still treat the small-scale processes as well. A great variety of disparate processes, operating over a broad range of spatial and temporal scales, must therefore be incorporated into predictive models. Performing long integrations over global space scales, while including detailed representation of local-scale processes (and in the case of the carbon system, multi-disciplinary processes), poses a considerable computational challenge. as water cools or warms), and the biological pump . These two pumps are discussed in greater detail in the “Atmospheric Composition and Radiative Forcing”

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