Microphysical explanation of the RH‐dependent water affinity of biogenic organic aerosol and its importance for climate

A large fraction of atmospheric organic aerosol (OA) originates from natural emissions that are oxidized in the atmosphere to form secondary organic aerosol (SOA). Isoprene (IP) and monoterpenes (MT) are the most important precursors of SOA originating from forests. The climate impacts from OA are c...

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Detalles Bibliográficos
Autores principales: Rastak, N., Pajunoja, A., Acosta Navarro, J. C., Ma, J., Song, M., Partridge, D. G., Kirkevåg, A., Leong, Y., Hu, W. W., Taylor, N. F., Lambe, A., Cerully, K., Bougiatioti, A., Liu, P., Krejci, R., Petäjä, T., Percival, C., Davidovits, P., Worsnop, D. R., Ekman, A. M. L., Nenes, A., Martin, S., Jimenez, J. L., Collins, D. R., Topping, D.O., Bertram, A. K., Zuend, A., Virtanen, A., Riipinen, I.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2017
Materias:
Research Letters
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5518298/
https://www.ncbi.nlm.nih.gov/pubmed/28781391
http://dx.doi.org/10.1002/2017GL073056

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5518298/
https://www.ncbi.nlm.nih.gov/pubmed/28781391
http://dx.doi.org/10.1002/2017GL073056

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