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biomass burning, fossil fuels, landfills and waste, and termites (see, e.g., Fung et al., 1991). the changes in methane may have been responding, at least in part, to changes in soil moisture and wetland extent , driven by re-organizations of the climate system. Although the precise nature of the mechanisms that have caused temperature and methane to co-vary in the past are somewhat uncertain, theseAmazing vintage sunflower canvas full printing low top shoes paleorecords indicate the possibility that temperature and methane may also co-vary in response to future climate changes. in the troposphere) warm the Earth’ s surface by trapping a portion of the outgoing longwave-radiation flux. Atmospheric aerosols tend to cause surface cooling by scattering solar radiation back into space , and they exert indirect effects by providing nucleation sites for the formation of cloud droplets. The net influence of the myriad feedbacks responding to changes in atmospheric gas and aerosol content has yet to be determined. Better understanding of these climatic influences will be fundamental to our ability to predict the nature and magnitude of the climate’ s response to anthropogenic change in any of the forcing factors. In each of the six sections of this chapter, the discussion is partitioned into

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