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A Mechanism for Halogen Release from Sea-Salt Aerosol in the Remote Marine Boundary Layer

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Abstract

Recent measurements of inorganic chlorine gases [1] and hydrocarbons [2] indicate the presence of reactive chlorine in the remote marine boundary layer; reactions involving chlorine and bromine can affect the concentrations of ozone, hydrocarbons and cloud condensation nuclei.

This text was first published as “A mechanism for halogen release from sea-salt aerosol in the remote marine boundary layer”, as: “Letter to Nature”, in: Nature, vol. 383, 26 September 1996: 327–330. The permission to republish this article was granted on 19 August 2015 by Ms. Claire Smith, Nature Publishing Group & Palgrave Macmillan, London, UK. The authors thank C. Brühl for calculating photolysis rate constants and B. Luo for calculating activity coefficients. This work was supported by the Deutsche Forschungsgemeinschaft.

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Vogt, R., Crutzen, P.J., Sander, R. (2016). A Mechanism for Halogen Release from Sea-Salt Aerosol in the Remote Marine Boundary Layer. In: Crutzen, P., Brauch, H. (eds) Paul J. Crutzen: A Pioneer on Atmospheric Chemistry and Climate Change in the Anthropocene. SpringerBriefs on Pioneers in Science and Practice(), vol 50. Springer, Cham. https://doi.org/10.1007/978-3-319-27460-7_8

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