Abstract
The paper is to study in wind tunnel on the flow and plume dispersion in the coastal region with complex terrain. Tufts visualization results show that the wind field of mean flow direction which revealed how the winds were flowing over the hilly terrain model for various wind directions. The reversed flows are observed at the region of the leeside of main hills or mountains of the terrain model. The plume averaged height increases with increasing the topography change parameter of the complex terrain. As the topography of terrain changes from flat terrain type to complex terrain type, the plume vertical dispersion parameter becomes greater.
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