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oceanic, surface, and subsurface reservoirs is likely being significantly affected as large amounts of groundwater are withdrawn and deposited in the other reservoirs.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 water vapor, cloudiness, and regional precipitation are largely unknown. Estimates of the mean annual fluxes, reservoirs, and processes associated with the global New version book lovers reading books and more books all over printed tote baghydrologic cycle are hard won and still relatively uncertain, and the year-to-year variability of the global cycle is poorly known. Not surprisingly, there is a paucity of information documenting the long-term variability of the hydrologic cycle. Variability is more easily documented locally than at larger scales; it shows up as variability of precipitation, but also as variability of water storage and runoff. While there is everywhere a fast component of rainfall variability because of the short time scales of the atmospheric hydrologic cycle, here we are more interested in the slower changes. Proxies for precipitation can be used to give a global view of precipitation processes and variability . For very long time records (e.g., 100 years), however, station data for precipitation must be used, because most

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