The four dimensional equations express mass conservation, momentum balance with pressure, gravity and viscous stress, heat advection and conduction, and a linear thermal-expansion equation of state. For heating from below, suitable plate conditions are and at , and , at . No slip and thermal insulation on the sidewall provide one suitable lateral completion; prescribed lateral temperatures would be another specified thermal setup.
Let be thermal diffusivity and kinematic viscosity. Use , , and as length, time, velocity and temperature scales. Subtract the static reference pressure with and scale its remainder by . Then
Density becomes . Substitution and division by the corresponding diffusion/viscous scales give
In the Boussinesq small-density-contrast limit retain buoyancy while neglecting the other factors. At infinite Prandtl number, after any fast initial adjustment, the equations are
The velocity is instantaneously constrained by a viscous elliptic balance; the temperature still evolves.
Take the divergence of the vector Poisson equation. Derivatives commute, and divergence of a curl is zero, so . Its boundary value is zero, hence the maximum principle gives throughout . The vector identity now gives , or
The layer domain is simply connected because its horizontal section is simply connected. For a curl-free field on such a domain, define as its line integral from a fixed base point to . Contractibility of loops and Stokes theorem make the integral path independent, and differentiation gives its gradient equal to the field. Thus .
Incompressibility then gives , while the prescribed normal curl gives . Green's identity yields
Hence is constant on the connected domain and . The extra condition belongs to the stated potential boundary problem; the reconstruction argument above uses the divergence and normal-curl conditions. On a multiply connected domain a curl-free field need not be a globally single-valued gradient.
Finally . Taking the curl of the infinite-Prandtl momentum balance and using gives
The derivation is an instance of velocity reconstruction from a mixed-boundary vector Poisson problem.