A nocturnal atmospheric loss of CH(2)I(2) in the remote marine boundary layer

Ocean emissions of inorganic and organic iodine compounds drive the biogeochemical cycle of iodine and produce reactive ozone-destroying iodine radicals that influence the oxidizing capacity of the atmosphere. Di-iodomethane (CH(2)I(2)) and chloro-iodomethane (CH(2)ICl) are the two most important or...

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Detalles Bibliográficos
Autores principales: Carpenter, Lucy J., Andrews, Stephen J., Lidster, Richard T., Saiz-Lopez, Alfonso, Fernandez-Sanchez, Miguel, Bloss, William J., Ouyang, Bin, Jones, Roderic L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6991967/
https://www.ncbi.nlm.nih.gov/pubmed/32055083
http://dx.doi.org/10.1007/s10874-015-9320-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6991967/
https://www.ncbi.nlm.nih.gov/pubmed/32055083
http://dx.doi.org/10.1007/s10874-015-9320-6

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