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      Size-segregated measurements of particulate elemental carbon and aerosol light absorption at remote arctic locations

      Atmospheric Environment (1967)
      Elsevier BV

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          Absorption coefficient of atmospheric aerosol: a method for measurement.

          Recent models predict that the effect of atmospheric aerosol particles on global temperature depends in part on b(abs,)or on n(2), where b(abs) is the aerosol absorption coefficient, and n(2) is the imaginary part of the aerosol refractive index for radiation in visible wavelengths. Satisfactory techniques for measuring b(abs) have yet to be developed. A method for measurement of b(abs) is described and discussed. The apparatus uses a piece of opal glass to integrate light scattered by particles collected on Nuclepore filters. It is quite mobile, inexpensive, and can be calibrated. Analysis of the errors inherent in the measurement shows it is accurate to well within an order of magnitude for particles of radius larger than 0.1 microm.
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            ON THE ORIGIN AND TRANSPORT OF THE WINTER ARCTIC AEROSOL

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              Soot in the Arctic

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                Author and article information

                Journal
                Atmospheric Environment (1967)
                Atmospheric Environment (1967)
                Elsevier BV
                00046981
                January 1982
                January 1982
                : 16
                : 10
                : 2461-2469
                Article
                10.1016/0004-6981(82)90136-6
                91b183a3-0e25-446f-9d9d-fa79c0a80a5d
                © 1982

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

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