Abstract
Aerosols have a climate impact through aerosol–radiation interactions and aerosol–cloud interactions, but can also interact with a number of biogeochemical cycles and have an impact on ecosystems. Physical and biological processes are sources of aerosols that can be modified by climate change, allowing for the possibility for climate feedback loops that can play a role in natural climate variability. This chapter provides a short description of some of the processes involved in these biogeochemical effects, such as the impact of aerosols on diffuse radiation at the surface and photosynthesis by terrestrial ecosystems, deposition of nutrients, and acidification. It is followed by a discussion of possible feedback loops involving aerosols, looking separately at the different aerosol species such as sulphate aerosols from dimethylsulphide, sea spray, secondary organic aerosols, biomass burning aerosols, and desert dust.
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Further Reading (Textbooks and Articles)
Fischer H, Siggaard-Andersen M-L, Ruth U, Röthlisberger R, Wolff E (2007) Glacial/interglacial changes in mineral dust and sea-salt records in polar ice cores: sources, transport, and deposition. Rev Geophys 45:RG100–2. doi:10.1029/2005RG000192
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Boucher, O. (2015). Biogeochemical Effects and Climate Feedbacks of Aerosols. In: Atmospheric Aerosols. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-9649-1_11
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