In practice, if the ambient fluids are stratified, the plume dynamics are dramatically different, due to the existence of a very sharp transition layer. These modifications are crucial to environmental scientists because of the consequential trapping phenomena, in which discharged pollutants are confined away from mixing flows, and may lead to hazardous air and water quality.
The UNC Fluids Lab is currently conducting expriments and running numerical simulations, to evaluate, verify and further improve various existing mathematical models that tried to explain these phenomena.
This is an abstract of a poster to be presented at the
2004 SEAMS Workshop in Charleston, SC. For more information, visit
the workshop's homepage at math.cofc.edu/SEAMS.