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water vapor, cloudiness, and regional precipitation are largely unknown. Estimates of the mean annual fluxes, reservoirs, and processes associated with the global hydrologic 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 Badass version carp fishing all over print stainless steel tumblerbe 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 relevant satellite-based observations extend back little more than a decade into the past. An investigation of the adequacy of the U.S. and southern Canadian station networks by Groisman and Easterling has shown that useful climatological information and statistics

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