Drivers of diel and regional variations of halocarbon emissions from the tropical North East Atlantic
Methyl iodide (CH<sub>3</sub>I), bromoform (CHBr<sub>3</sub>) and dibromomethane (CH<sub>2</sub>Br<sub>2</sub>), which are produced naturally in the oceans, take part in ozone chemistry both in the troposphere and the stratosphere. The significance of oceanic upwelling regions for emissions of these...
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| Principais autores: | , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Copernicus Publications
2014-02-01
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| Series: | Atmospheric Chemistry and Physics |
| Acceso en liña: | http://www.atmos-chem-phys.net/14/1255/2014/acp-14-1255-2014.pdf |
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