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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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Bibliografske podrobnosti
izdano v:Geophys Res Lett
Main Authors: 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.
Format: Artigo
Jezik:Inglês
Izdano: John Wiley and Sons Inc. 2017
Teme:
Online dostop:https://ncbi.nlm.nih.gov/pmc/articles/PMC5518298/
https://ncbi.nlm.nih.gov/pubmed/28781391
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017GL073056
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