Substantial large-scale feedbacks between natural aerosols and climate

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Direct radiative feedback due to biogenic secondary organic aerosol estimated from boreal forest site observations

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Nitrogen Availability Reduces CMIP5 Projections of Twenty-First-Century Land Carbon Uptake*

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Climate-induced variations in global wildfire danger from 1979 to 2013

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Human land-use-driven reduction of forest volatiles cools global climate

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Natural aerosol direct and indirect radiative effects

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Warming-induced increase in aerosol number concentration likely to moderate climate change

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Evolution of anthropogenic and biomass burning emissions of air pollutants at global and regional scales during the 1980–2010 period

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Biogenic carbon and anthropogenic pollutants combine to form a cooling haze over the southeastern United States

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Improvements to NOAA’s Historical Merged Land–Ocean Surface Temperature Analysis (1880–2006)

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Predicted change in global secondary organic aerosol concentrations in response to future climate, emissions, and land use change

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