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 . Then
and the equations become
Equivalently, the ordinary differential equations for the three unknowns are
The 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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