When and are constant, eliminating height between and gives . Thus is constant. Its sign classifies forced and lazy departures from pure plume balance, and its vanishing makes a finite-source plume exactly self-similar after a virtual-origin shift.
For positive source fluxes and positive constant buoyancy flux, the plume flux-balance invariant has a finite constant while grows without bound. Dividing by makes the source imbalance vanish relatively. The balances then give and . This attraction concerns relative similarity and does not assert that different finite sources share the same virtual origin.

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