Rayleigh–Bénard Convection

After the first display, valid Ra or roll-count edits update the illustration immediately and pause the direction markers. Only exact Ra text and the selected number of pairs are retained; no image or marker phase is saved. Examples are in the menu; Reset restores Ra2500 and two pairs. Reference onset and prescribed-field explanations are available in tooltips and this help.

Reference onset. Ra = g β ΔT H³ / (ν κ), with gravity g, expansion coefficient β, plate temperature difference ΔT, depth H, kinematic viscosity ν and thermal diffusivity κ. Ra_c ≈ 1708 is the rounded linear onset for the classical non-rotating Boussinesq layer between two rigid, no-slip, isothermal horizontal plates, with an unbounded horizontal extent. It is not a universal threshold for any container or boundary condition. The rounded threshold is used as this illustration’s switch: no flow at or below 1708. See Kao & Yang, 2007.

What is drawn. z runs from 0 at the hot bottom to 1 at the cold top; x is measured in layer depths. Temperature θ = (T − T_top) / ΔT has fixed plate values 1 and 0. The prescribed streamfunction is ψ = I/π · sin(πx) sin²(πz). Its derivatives u = ∂ψ/∂z and w = −∂ψ/∂x give a divergence-free field with zero velocity at both plates. θ = 1 − z + 0.2w links warm departures from conduction to upward motion and cool departures to downward motion. Horizontal continuation is periodic.

Schematic intensity. I = min(1, √max(0, Ra/1708 − 1)) is a chosen visual mapping, not a predicted velocity or heat flux. It saturates at Ra = 3416. The controls cover Ra from 0 to 5000 solely for this demonstration. No Navier–Stokes, temperature evolution, Nusselt number or turbulent transition is calculated. The temperature pattern is stationary; direction markers move along its streamlines at an illustrative speed, with no physical time unit. Reduced-motion preferences start the markers paused.

View. One to four visible pairs show different lengths of the same periodic pattern. Their count is chosen, not predicted, and does not change the reference onset. Horizontal and vertical coordinates use the same scale. Long sections scroll within the diagram on narrow screens. The example does not resolve rigid side walls or calculate the critical wavelength. All computation stays in the browser.

Pause/Resume freezes or moves only the direction markers; temperature stays stationary. Hidden pinned tools freeze marker phase and resume without catching up. This is not physical elapsed time.