Take logarithmic height with an arbitrary fixed length , so . This is dimensionally meaningful and has the same derivatives as the abbreviated . For example,
The exponent vanishes and the coefficient is , by the plume similarity in power-law stratification. Likewise the momentum coefficient is and the buoyancy coefficient is . The logarithmic-height plume equations are therefore
The reference similarity solution becomes the equilibrium of an autonomous differential equation. Normalizing each flux by its own height-dependent similarity value is essential; simply differentiating the unnormalized fluxes would miss the three subtraction terms.

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