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only by anthropogenic changes, but also by natural variations in the sun’s output and by the input and distribution of volcanic aerosols. Largely unpredictable, these elements exert measurable influence over the Earth’s radiative budget and atmospheric chemical interactions, and account for some of the natural dec-cen variability in the Earth’s climate. Solar output, volcanic aerosol contributions, and atmospheric gases and aerosols thus represent the main New version book lovers reading nerd love all over printed tote bagforcings, natural and anthropogenic, of the climate system. In this respect, they are distinct from the components of the climate system discussed in the other sections of this chapter, and changes in them will drive responses in those other components. Ultimately we need to be able to differentiate climate variations driven by changes in the forcings from variations that are the expression of internal or coupled modes of variability, which will occur even when forcing is steady. Our efforts to understand the behavior of climate variations may be furthered by the fact that the forcings and responses may vary with latitude or regional characteristics, possibly relating specific forcings to specific responses or

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