A plume is a localized buoyancy-driven flow generated by a source of heat or another density-changing substance. A plume can be laminar or turbulent; the transport regime is an additional condition.
A laminar plume is a narrow buoyancy-driven flow in which viscous diffusion balances inertia across the plume.
For a steady incompressible plume with localized vertical body force , decay of velocity and shear at transverse infinity gives
If , balancing the momentum flux and transverse viscosity gives
With , , , and , the plume boundary-layer equation reduces to

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