This paper studies the two-dimensional inhomogeneous Navier–Stokes equations governing stratified flows in a bounded domain under a gravitational potential . Our main results are as follows. First, we provide a rigorous characterization of steady states, proving that under the Dirichlet condition , all admissible equilibria are hydrostatic and satisfy . Second, through a perturbative analysis around arbitrary hydrostatic profiles, we show that despite possible transient growth induced by the Rayleigh–Taylor mechanism, the system always relaxes to a hydrostatic equilibrium. Third, we identify a necessary and sufficient condition on the initial density perturbation for convergence to a linear hydrostatic density profile of the form , with and . Finally, we establish improved regularity estimates for strong solutions corresponding to initial data in the Sobolev space .

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