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      Towards the development of a global inventory for black carbon emissions

      , ,
      Atmospheric Environment. Part A. General Topics
      Elsevier BV

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          Climate forcing by anthropogenic aerosols.

          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 climate forcing due to anthropogenic sulfate is estimated to be -1 to -2 watts per square meter, globally averaged. This perturbation is comparable in magnitude to current anthropogenic greenhouse gas forcing but opposite in sign. Thus, the aerosol forcing has likely offset global greenhouse warming to a substantial degree. However, differences in geographical and seasonal distributions of these forcings preclude any simple compensation. Aerosol effects must be taken into account in evaluating anthropogenic influences on past, current, and projected future climate and in formulating policy regarding controls on emission of greenhouse gases and sulfur dioxide. Resolution of such policy issues requires integrated research on the magnitude and geographical distribution of aerosol climate forcing and on the controlling chemical and physical processes.
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            Biomass-burning emissions and associated haze layers over Amazonia

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              Soot Carbon and Excess Fine Potassium: Long-Range Transport of Combustion-Derived Aerosols

              M. Andreae (1983)
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                Author and article information

                Journal
                Atmospheric Environment. Part A. General Topics
                Atmospheric Environment. Part A. General Topics
                Elsevier BV
                09601686
                June 1993
                June 1993
                : 27
                : 8
                : 1277-1295
                Article
                10.1016/0960-1686(93)90255-W
                ccb73b7f-b5b7-4515-a541-95565b929775
                © 1993

                http://www.elsevier.com/tdm/userlicense/1.0/

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