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anomalies for the two are significantly different from one another, indicating that the atmospheric circulation had changed considerably. The seasonal distribution of global mean temperature also attests to the importance of atmospheric circulation in climate variability (see Wallace et al., 1993). the first six months), warmed this region of the atmosphere by a few degrees. Following the eruption of Mt. Pinatubo, substantial changes to the planetary albedo were observed (Minnis et al., 1993). In addition, substantial heating in the tropical stratosphere was observed immediately after Pinatubo’s eruption. This heating was sufficient to cause tropical stratospheric temperatures at 30 hPa to increase as much as three standard deviations above the 26-year mean . On the other hand, global surface Hot vikings tattoo symbol all over print stainless steel tumblertemperature was also observed to decrease in the months following the Pinatubo eruption as a result of the increased planetary albedo (see, e.g., Dutton and Christy, 1992), and the temperature remained suppressed through 1993, as predicted (Hansen et al., 1996). Changes in solar output—either in terms of total radiative flux , or in terms of the spectral distribution of this radiation—will directly influence the radiative environment and energy budget at the Earth’s surface, the response of the climate system, and the response of many life forms. Moreover, changes in the atmospheric concentration of a number of trace constituents directly

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