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References                        161



































         Fig. 11-3. Stratospheric ozone and CIO concentrations at an altitude of 18 km measured
        by aircraft flying south over Antarctica on September 27,1987. The dramatic decrease in ozone
        at a latitude of 71 degrees is attributed to the role of CIO in catalytic destruction of ozone.
        Adapted from Anderson et al. (13).



        viewed for potential adverse effects on the atmosphere. In addition, other
        greenhouse gases will be subject to investigation and questioning of their
        role in global warming scenarios.




                                   REFERENCES
         1. Schneider, S. H., Bull. Am. Meteorol. Soc. 71, 1292-1304 (1990).
         2. Lindzen, R., Bull. Am. Meteorol. Soc. 71, 288-299 (1990).
         3. Kellogg, W. W., Bull. Am. Meteorol. Soc. 72, 499-511 (1991).
         4. Folland, C. K., Karl, T., and Vinnikov, K. Ya., Observed climate variations and change,
           in "Climate Change: The IPCC Scientific Assessment," Working Group 1 Report (J. T.
           Houghton, G. J. Jenkins, and J. J. Ephramus, eds.), pp 195-238. Cambridge University
           Press, Cambridge, 1990.
         5. Jones, P. D., /. Climatol. 1, 654-660 (1988).
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