The influence of ozone precursor emissions from four world regions on tropospheric composition and radiative climate forcing
| Autor: | Guang Zeng, Elina Marmer, William J. Collins, Oliver Wild, Cyndi Atherton, M. Daniel Schwarzkopf, Drew Shindell, Sophie Szopa, Daniel Bergmann, Vaishali Naik, Bryan N. Duncan, Meridith M. Fry, Martin G. Schultz, J. Jason West, Ian A. MacKenzie, Arlene M. Fiore, Frank Dentener, Peter Hess |
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| Rok vydání: | 2012 |
| Předmět: |
Atmospheric Science
Ozone 010504 meteorology & atmospheric sciences Soil Science Climate change 010501 environmental sciences Aquatic Science Oceanography Atmospheric sciences 01 natural sciences Troposphere chemistry.chemical_compound Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) NOx 0105 earth and related environmental sciences Earth-Surface Processes Water Science and Technology Ecology Global warming Paleontology Forestry Radiative forcing Geophysics chemistry 13. Climate action Space and Planetary Science Atmospheric chemistry Environmental science Water vapor |
| Zdroj: | Journal of Geophysical Research: Atmospheres. 117 |
| ISSN: | 0148-0227 |
| DOI: | 10.1029/2011jd017134 |
| Popis: | 0.4 2.6 to 1.9 1.3 Gg for NOx reductions, 0.1 1.2 to 0.9 0.8 Gg for NMVOC reductions, and 0.09 0.5 to 0.9 0.8 Gg for CO reductions, suggesting additional research is needed. The 100-year global warming potentials (GWP100) are calculated for the global CH4 reduction (20.9 3.7 without stratospheric O3 or water vapor, 24.2 4.2 including those components), and for the regional NOx, NMVOC, and CO reductions (18.7 25.9 to 1.9 8.7 for NOx, 4.8 1.7 to 8.3 1.9 for NMVOC, and 1.5 0.4 to 1.7 0.5 for CO). Variation in GWP100 for NOx, NMVOC, and CO suggests that regionally specific GWPs may be necessary and could support the inclusion |
| Databáze: | OpenAIRE |
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