Abstract
O'Dowd et al. reply - McFiggans1 raises some interesting, but partly speculative, issues about the possibility of additional condensable-iodine-vapour (CIV) precursors being involved in marine aerosol formation from biogenic iodine emissions, and about the relative roles of iodine oxide and sulphuric acid in the marine new-particle formation process.
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References
McFiggans, G. Nature doi:10.1038/nature03372 (2005).
O'Dowd, C. et al. Nature 417, 632–636 (2002).
Yoon, Y. J. et al. Proc. 16th Intl Conf. Nucleation and Atmospheric Aerosols, Kyoto (eds Kasahara, M. & Kulmala, M.) 674–677 (Kyoto University Press, 2004).
McFiggans, G. et al. Atmos. Chem. Phys. 4, 1–13 (2004).
Pirjola, L., O'Dowd, C. D., Brooks, I. M. & Kulmala, M. J. Geophys. Res. 105, 26531–26546 (2000).
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O'Dowd, C., Jimenez, J., Bahreini, R. et al. Marine aerosols and iodine emissions (Reply). Nature 433, E13–E14 (2005). https://doi.org/10.1038/nature03373
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DOI: https://doi.org/10.1038/nature03373
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