Oxidized organic aerosol is a major component of ambient particulate matter, substantially impacting climate, human health, and ecosystems. Oxidized aerosol from biomass burning is especially toxic, known to contain a large amount of species that are known carcinogens, mutagens. Inhaling biomass burning particles also cause oxidative stress and cause a wide range of diseases such as heart attacks, strokes, and asthma. Oxidized aerosol primarily forms from the atmospheric oxidation of volatile and semi-volatile compounds emitted by sources like biomass burning, resulting in products that readily form particulate matter. Every model in use today assumes that oxidized aerosol forms in the presence of sunlight, and that it requires days of atmospheric processing to reach the levels observed in the environment. Naturally this implies that oxidized aerosol forms in the daytime and mostly during periods with plentiful sunshine, such as in summer.
However, considerable amounts of oxidized organic aerosol forms during the wintertime and in other periods of low photochemical activity worldwide, often during periods of intense biomass burning. Models cannot capture this considerable source of oxidized aerosol, underestimating oxidized aerosol levels by a factor of 3-5. This unresolved and important mystery carries significant implications for public health and climate, given that biomass burning events often are associated with population exposure to very high particulate matter levels. This issue becomes ever more important in the future, given the increase intensity, duration and frequency of woodburning (both domestic and wildfire) throughout the globe.
Research lead by the teams of Prof. Athanasios Nenes and Spyros Pandis of the Center for Studies on Air Quality and Climate Change (C-STACC; http://cstacc.
The Kodros et al. study is broadly important for a number of reasons. First, it is shown beyond doubt that sunlight is not required to rapidly generate significant amounts of oxidized aerosol — which reshapes the understanding of how pollution from biomass burning is formed. Second, this mechanism can explain the paradoxically high levels of organic pollution in urban environments during wintertime haze episodes, such as in Europe and China. Finally, the work greatly elevates the role of biomass burning as a source of air pollution at night, in winter, and during other periods of low solar activity — where intense haze episodes often seen to occur throughout the world.
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