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contributor authorCovert, D. S.
contributor authorCharlson, R. J.
contributor authorAhlquist, N. C.
date accessioned2017-06-09T17:23:03Z
date available2017-06-09T17:23:03Z
date copyright1972/09/01
date issued1972
identifier issn0021-8952
identifier otherams-8422.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227534
description abstractA chemically pure aerosol of defined size distribution exhibits a unique growth pattern due to adsorption of water vapor, and to hygroscopic and/or deliquescence effects which are dependent upon relative humidity and which can be followed by measuring light scattering by the aerosol. A number of pure aerosols were produced artificially in the laboratory, subjected to a controlled humidity environment, and the magnitude of their light scattering coefficient measured continuously over a wide range of relative humidity (20?90%) with an integrating nephelometer. The results obtained can be applied to similar measurements on ambient air to yield qualitative chemical information and to determine the amount of visibility degradation which may be attributed to the association of water vapor with atmospheric aerosols. Examples of light scattering-relative humidity relationships for atmospheric aerosols are given.
publisherAmerican Meteorological Society
titleA Study of the Relationship of Chemical Composition and Humidity to Light Scattering by Aerosols
typeJournal Paper
journal volume11
journal issue6
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1972)011<0968:ASOTRO>2.0.CO;2
journal fristpage968
journal lastpage976
treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 006
contenttypeFulltext


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