Halogen chemistry reduces tropospheric O<sub>3</sub> radiative forcing
Tropospheric ozone (O<sub>3</sub>) is a global warming gas, but the lack of a firm observational record since the preindustrial period means that estimates of its radiative forcing (RF<sub>TO<sub>3</sub></sub>) rely on model calculations. Recent observational evid...
Main Authors: | T. Sherwen, M. J. Evans, L. J. Carpenter, J. A. Schmidt, L. J. Mickley |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-01-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | http://www.atmos-chem-phys.net/17/1557/2017/acp-17-1557-2017.pdf |
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