Write the background mass density as and its hydrostatic pressure as , whereApply an Eulerian perturbation of a fluid variable to the background fields:Thus is the Eulerian pressure perturbation, in pascals; it is not the background hydrostatic pressure.
For incompressible flow, mass conservation becomes . Linearizing about rest givesThe Euler equations are . The background pressure gradient and weight cancel. Dropping products of perturbations givesUnder , replace by in inertia but retain the background mass density gradient in the displacement-induced buoyancy. This is the Boussinesq approximation. Its linear Boussinesq equations here areThe absolute value makes explicit that the small-density-variation condition concerns magnitude, including the usual negative of stable density stratification.
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