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: | , , , , |
|---|---|
| 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 |