Vol. 13, issue 06-07, article # 3
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Abstract:
We study the dynamic characteristics of a volcanic plume that is being a vertical cylindrical convective jet above a crater depending on the intensity of aerosol emission, particle size, and density of the particulate matter. In computations, the nonstationary numerical model of a convective jet is used. It is shown that the rate of the convective flow decreases with the increasing intensity of aerosol emission.