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predictable. Our understanding of the influence of tropospheric aerosols on dec-cen climate-change problems is, in general, woefully inadequate, and requires considerable attention to identify the most important aspects. The source and sinks of anthropogenic radiatively active gases remain a primary concern in determining the extent of the effect of greenhouse gases on global climate. However, an equally important influence on climate is the distribution of increased atmospheric water vapor associated with a speeding up of the hydrologic cycle . The atmospheric portion of the hydrologic cycle is complex, and operates on both short and long time scales. The fast processes associated with this mechanism, such as cloud formation and the related intra-and inter-cloud radiative impacts, influence The hottest version moose hunting camo version all over print stainless steel tumblercloud nucleation, longwave radiation, albedo feedbacks, and ultimately the surface energy balance. On dec-cen time scales, the impact of increased water vapor is realized through alterations in large-scale cloud distribution (shown earlier in Figure 2-12), which reflect both the water-vapor distribution and the hydrologic cycle’s response. Also, the latent heating of clouds, and its radiative effects, influence the large-

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