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solar variability is still being debated. Even studies that point to apparently distinct influences of solar variability on climate often indicate highly variable sensitivities for a given change in irradiance. Feedbacks in the climate system, particularly the atmosphere, may account for enhancement or damping of the climatic response to Amazing baby bear with heart all over printed slipperssolar forcing. Understanding the sensitivity of the Earth’s climate to past changes in solar activity will permit better predictions of future changes in the face of decadally varying solar irradiance. It will also suggest potential responses associated with other sources of change in the radiative forcing (e.g., internal sources, such as changing albedo). • How does the coupling between chemistry, dynamics, and radiation in the lower stratosphere and upper troposphere operate on dec-cen time scales? For example, what do we need to know in order to predict accurately the timing of stratospheric ozone recovery from anthropogenic halo-carbon depletion? How and by what mechanisms do changes in the stratosphere affect atmospheric circulation and the surface radiation balance on longer time scales, recognizing that much of the

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