Climate Forcing by Anthropogenic Aerosols

  title={Climate Forcing by Anthropogenic Aerosols},
  author={Robert J. Charlson and Stephen E. Schwartz and Jeremy M. Hales and Robert D. Cess and James A. Coakley and Jeff Hansen and David J. Hofmann},
  pages={423 - 430}
Although long considered to be of marginal importance to global climate change, tropospheric aerosol contributes substantially to radiative forcing, and anthropogenic sulfate aerosol in particular has imposed a major perturbation to this forcing. Both the direct scattering of shortwavelength solar radiation and the modification of the shortwave reflective properties of clouds by sulfate aerosol particles increase planetary albedo, thereby exerting a cooling influence on the planet. Current… 

Aerosols, Clouds, and Climate Change

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Anthropogenic sulfate (SO 4 = ) aerosol particles play two potential roles in the radiative climate of the earth. In cloud-free air, SO 4 = particles scatter sunlight, some of which is lost to space,

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VARIOUS mechanisms have been suggested whereby clouds might take part in or initiate climate change, including changes in cloud amounts, liquid-water paths and droplet sizes1–11. Previous studies of

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RECORDS of sulphate and nitrate concentrations in ice cores show that these concentrations have increased recently because of the long-range transport of pollution from middle latitudes1–5. But these

Increase in the Stratospheric Background Sulfuric Acid Aerosol Mass in the Past 10 Years

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Data obtained from measurements of the stratospheric aerosol at Laramie, Wyoming (41�N), indicate that the background or nonvolcanic stratospheric sulfuric acid aerosol mass at northern mid-latitudes

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