The U.S. Climate Change Science Program is in the process of producing 21 draft assessments that investigate changes in the Earth’s climate and related systems. These assessments are designed to inform decisionmakers about the scientific underpinnings of a range of environmental issues, such as stratospheric ozone. This National Research Council report reviews one of these assessments, Synthesis and Assessment Product (SAP) 2.4, Trends in Emissions of Ozone Depletion Substances, Ozone Layer Recovery, and Implications for Ultraviolet Radiation Exposure. This assessment is noted as being the first-ever attempt to look at the United States contribution to ozone-depleting substances and ozone recovery. This National Research Council book commends the assessment’s authoring team for comprehensively covering the scientific basis of ozone and ozone-depleting substances, but recommends several ways that the assessment could be improved. Suggestions include clarifying the discussion on climate effects of ozone and revising the approach to estimating U.S. contributions to production, consumption, and emission of ozone-depleting substances. The assessment could also be improved by reorganizing and editing to accommodate intended audiences.
Board on Atmospheric Sciences and Climate & Committee to Review the U.S. Climate Change Science Program’s Draft Synthesis and Assessment Product 2.4
Review of the U.S. Climate Change Science Program’s Draft Synthesis and Assessment Product 2.4 [PDF ebook]
Trends in Emissions of Ozone Depleting Substances, Ozone Layer Recovery, and Implications for Ultraviolet Radiation Exposure
Review of the U.S. Climate Change Science Program’s Draft Synthesis and Assessment Product 2.4 [PDF ebook]
Trends in Emissions of Ozone Depleting Substances, Ozone Layer Recovery, and Implications for Ultraviolet Radiation Exposure
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भाषा अंग्रेज़ी ● स्वरूप PDF ● पेज 74 ● ISBN 9780309115261 ● प्रकाशक National Academies Press ● प्रकाशित 2007 ● डाउनलोड करने योग्य 3 बार ● मुद्रा EUR ● आईडी 7140998 ● कॉपी सुरक्षा Adobe DRM
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