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confirmed with high statistical significance in much longer proxy records having annual resolution (Quinn et al., 1996; Biondi et al., 1997), as well as in the longest available instrumental record (Plaut et al., 1995). The spatial patterns and physical mechanisms associated with these broad spectral peaks are the focus of intense current research. Thus the 13-to-15-year peak has been associated with variability of the North Atlantic current system (Sutton and Amazing vintage sunflower full printing low top shoesAllen, 1997; Moron et al., 1998), while the 20-to-25-year peak has been associated with oscillations in the thermohaline circulation (Delworth et al., 1993; Chen and Ghil, 1996). This section focuses on those aspects of the atmospheric circulation that need to be understood and modeled in order to properly represent the interaction of the atmosphere with the other components of the climate system, and to better identify and understand its unique role in these interactions. Water vapor is treated in the “Hydrologic Cycle” section that follows this one. The contributions of the slower components of the climate system, which are most responsible for driving the dec-cen variability manifested in the atmospheric circulation and the hydrologic cycle, are presented in the last

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