Take inward fluid entrainment speed to be positive. The non-Boussinesq form of the Batchelor entrainment hypothesis is
where is the entrainment coefficient. Define physical, cross-section-integrated fluxes for the top-hat plume model by
Thus is mass flux, is momentum flux, and is a density-weighted buoyancy flux. The kinematic buoyancy flux in the Boussinesq approximation is . These definitions keep the factor ; conventions suppressing it simply rescale all three fluxes consistently.
For a homogeneous ambient, the sectional volume, mass and momentum balances are
The momentum source is the net upward buoyancy force; entrained ambient fluid initially supplies no vertical momentum. Subtracting the mass balance from times the volume balance gives conservation of the density deficit:
Now , , and . Substitution produces the non-Boussinesq top-hat plume equations
For reconstructing the fields without a Boussinesq approximation,
The last expression uses the plume density in the acceleration denominator; it agrees with the ambient-density definition of reduced gravity to Boussinesq order.
Use the kinematic fluxes , and . In the steady Boussinesq approximation, the non-Boussinesq top-hat plume equations reduce to
Eliminating gives , where the integration constant vanishes for a pure plume from a point source. Write and . The two balances give and . The Boussinesq point-source plume is therefore
Here and tend to zero at the source, while remains positive. The plume Froude number is independent of height:
The ideal point source is a far-field similarity idealization. Since , the Boussinesq approximation fails near and is valid only when . In terms of , this requires ; the density formula must not be extrapolated into its unphysical negative-density region.