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References
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[5] The Future and Recovery." In Trends in Emissions of Ozone-Depleting Substances, Ozone Layer Recovery, and Implications for Ultraviolet Radiation Exposure, edited by A. R. Ravishankara, M. J. Kurylo and C. A. Ennis, 133-154. Vol. Synthesis and Assessment Product 2.4. Asheville, NC: NOAA's National Climatic Data Center, 2008.
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[3] Changes in Atmospheric Constituents and in Radiative Forcing." In Climate Change 2007: The Physical Basis, edited by S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor and H. L. Miller, 129-234. Vol. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, UK and New York, NY: Cambridge University Press, 2007.
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[46] Executive Summary." In Temperature Trends in the Lower Atmosphere: Steps for Understanding and Reconciling Differences, edited by T. R. Karl, S. J. Hassol, C. D. Miller and W. L. Murray, 1-15. Vol. Synthesis and Assessment Product 1.1. Washington, D.C.: U.S. Climate Change Science Program, 2006.
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[63] Why Do Temperatures Vary Vertically (from the Surface to the Stratosphere) and What Do We Understand About Why They Might Vary and Change Over Time?" In Temperature Trends in the Lower Atmosphere: Steps for Understanding and Reconciling Differences, edited by T. R. Karl, S. J. Hassol, C. D. Miller and W. L. Murray, 15-28. Vol. Synthesis and Assessment Product 1.1. Washington, D.C.: U.S. Climate Change Science Program, 2006.
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