Aviation and the Global Atmosphere

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Figure 6-10: Radiative forcing (dotted line), global mean surface temperature change including all internal feedback processes (dashed line), and climate sensitivity parameter l (solid line) from 100 DU additional ozone as a function of altitude (model layer) to which ozone was added. The plot is based on results of a simplified GCM (data from Table 3 by Hansen et al., 1997b).

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