Atmosphere | |
Atmospheric Ozone and Methane in a Changing Climate | |
Ivar S. A. Isaksen3  Terje K. Berntsen3  Stig B. Dalsøren5  Kostas Eleftheratos2  Yvan Orsolini1  Bjørg Rognerud3  Frode Stordal3  Ole Amund Søvde5  Christos Zerefos4  | |
[1] NORWEGIAN Institute for Air Research (NILU), N-2027 Kjeller, Norway; E-Mail:;Department of Geology and Geoenvironment, University of Athens, 15784 Athens, Greece; E-Mail:;Department of Geosciences, University of Oslo, N-0315 Oslo, Norway; E-Mails:;Academy of Athens, 10680 Athens, Greece; E-Mail:;Center for International Climate and Environmental Research—Oslo (CICERO), N-0318 Oslo, Norway; E-Mails: | |
关键词: ozone; methane; atmospheric processes; chemistry; dynamics; Quasi Biennial Oscillation (QBO); permafrost; | |
DOI : 10.3390/atmos5030518 | |
来源: mdpi | |
【 摘 要 】
Ozone and methane are chemically active climate-forcing agents affected by climate–chemistry interactions in the atmosphere. Key chemical reactions and processes affecting ozone and methane are presented. It is shown that climate-chemistry interactions have a significant impact on the two compounds. Ozone, which is a secondary compound in the atmosphere, produced and broken down mainly in the troposphere and stratosphre through chemical reactions involving atomic oxygen (O), NO
【 授权许可】
CC BY
© 2014 by the authors; licensee MDPI, Basel, Switzerland.
【 预 览 】
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RO202003190023322ZK.pdf | 835KB | download |