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system’ s radiative response to anthropogenic increases in greenhouse gases , and to reliably estimating the green-house-warming response. • How do the distribution of water vapor, precipitation, and clouds respond to and interact with surface boundary conditions and changes in forcings on dec-cen time scales? The hydrologic cycle plays a poorly defined role in producing and responding to the patterns of climate variability we have identified in Chapter 3. These patterns and large-scale precipitation seem to co-vary, however, so efforts to use Premium carp fishing all over print stainless steel tumblerknowledge of climate patterns to predict regional precipitation should be enhanced. There is clearly a need for better documentation and understanding of the nature and sensitivity of these co-varying relationships, and for establishing and refining the mechanisms responsible for driving them. ), such as the Ogallala aquifer in the central United States. These human and natural processes affect stream-aquifer interactions on dec-cen time scales. Moreover, the temporal distribution of the global hydrologic budget between the atmospheric, oceanic, surface, and subsurface reservoirs is likely being significantly affected as large amounts of groundwater are withdrawn and deposited in the other reservoirs. The resultant impacts on atmospheric

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