Abstract
The intent of this paper is to present, from a meteorologist’s viewpoint, a brief review of the processes responsible for transforming and removing pollutants from the atmosphere. Such processes include dry deposition, precipitation scavenging, and chemical and physical transformations; and to facilitate the meteorology-oriented nature of this presentation, we shall discuss them here within the framework of the familiar equations of mass continuity. For conservation of pollutant mass in the gas phase (in air, that is), these equations are
(A = component index = 1, 2, ..., N; y signifies “gas phase” where the time rate of change of airborne pollutant concentration is related to the divergence and source-sink terms in the conventional manner. Here we are interested primarily in rAy and wA, which we shall call the “gas-phase reaction*” and “interphase transport” terms, respectively, rAy accounts for all chemical and physical reaction that occurs in the gas phase, and wA depicts the loss of material by the gas phase via transport to the aqueous phase, (i.e., rain, snow, fog, ...). One should note here the consistency of units of rAy and wA, which are mass/volume • time.
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Halest, J.M. (1982). Atmospheric Transformations of Pollutants. In: Lectures on Air Pollution and Environmental Impact Analyses. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-935704-23-2_7
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DOI: https://doi.org/10.1007/978-1-935704-23-2_7
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