We obtain solutions for a vertical buoyant jet in a crossflow
And buoyant jets discharged horizontally perpendiculat to crossflow.
z/Lb =cxy(x/Lm)1/3 (5)
This model performs satisfactorily for simple flows with no shoreline interaction or attachment. Strong crosscurrents or limited depths causing attachment with the downstrean bank or strong initial buoyancy render this model invalid. In addition, they are incapable of simulating any far-field processes that occur after a certain distance. If the z-coordinate of the plume centerline z_cl is higher than then water surface z_ws, the algorithm takes z_cl=z_ws.
Canarina DESCAR software · oceanographic pollution · algorithms 5
It is interesting for BMP, traffic noise, noise prediction, noise prediction software, oceanographic