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Between 2005 and 2012, US emissions of nitrogen oxides (NO ) and sulfur dioxide (SO ) decreased by 42% and 62%, respectively. These species, as well as ammonia (NH ), are precursors of inorganic fine aerosols, which scatter incoming shortwave radiation and thus affect climate. Scaling aerosol concentrations to emissions, as might be done for near-term climate projections, neglects nonlinear chemical interactions.
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