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as well as atmospheric and oceanic circulation. For instance, atmospheric circulation helps determine the convergences and divergences of vapor , but the condensation processes in turn help determine the circulation of the atmosphere. exchange of heat, moisture, and momentum) and feedbacks, need to be better understood. Much of the dec-cen variability in the atmospheric circulation arises through interactions and coupling with the boundaries, yet this complex interface region is poorly understood, and poorly resolved in models. Because of climate models’ The hottest version vikings tattoo symbol all over print stainless steel tumblerrelatively coarse vertical resolution, the dynamics of this interaction cannot be resolved in models, so they must be parameterized in terms of large-scale circulation quantities. Our ability to correctly model the atmospheric response to greenhouse-gas increases and to natural surface-temperature and moisture anomalies, as well as the ability to correctly force ocean models, depend on boundary-layer processes. Finally, the processes controlling the large-scale wave features and their interaction with the major climate patterns described in Chapter 3, including such shorter-time-scale features as ENSO, must be better understood to be correctly represented in models. The study of dec-cen variability of the atmospheric circulation faces many challenges. The widespread current interest in

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