Abstract
The characteristics of vertical forced plume in a uniform cross flow of stably linear stratified environment are studied both numerically and experimentally. The empirical formulas for the diffusion characteristics of vertical forced plume (trajectory, dilution, etc.) are presented experimentally. The three-dimensional numerical model is used to quantitatively simulate the behavior of the vertical forced plume in these ambient conditions. The performance of the three-dimensional model is evaluated by comparison of numerical results with experimental measurements. By using numerical model, the production and disappearance of vortex pairs are discussed as plume flow downstream.
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