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A B S T R A C T Regional aerosol concentrations are governed by an evolving balance between aerosol sources and sinks. Here, a simple technique is described for making estimates of the extent to which seasonal aerosol variability is controlled by wet scavenging rather than the efficiency of transport from pollution source regions. Carbon monoxide (CO) is employed as an assumed passive tracer of pollution transport efficiency, to which the magnitude of aerosol light scattering is compared.doi:10.1111/j.1600-0889.2010.00453.x fatcat:xeyxgpipc5elvb2fckjksvlxtu