In the top-hat plume model, vertical velocity and reduced gravity are uniform over . The ambient has zero vertical velocity, negligible ambient turbulence and a prescribed . Thenand the equations becomeEquivalently, the ordinary differential equations for the three unknowns areThe last equation displays dilution by fluid entrainment as well as loss of relative buoyancy while rising through a stably stratified ambient. The model assumes a steady slender two-dimensional turbulent plume, large Reynolds number, the Boussinesq approximation, constant and , negligible heat loss, negligible imposed crossflow, and negligible pressure departure from ambient hydrostatic pressure. The factors of two count both entraining edges; is a half-width. A finite source also requires its volume, momentum and buoyancy fluxes as boundary data.
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