Buoyancy, damping and geometry
The selected horizontal wave number minimizes onset for stress-free isothermal boundaries. Rigid walls have a different threshold.
Fluid dynamics · from rolls to chaos
Integrate three convection modes from a small perturbation. Orbit the hot–cold exchange and tracer paths; connect temperature profiles, heat transport and phase-space trajectories as steady rolls form and lose stability.
Physics tutorial
BackgroundHeating from below makes the lower fluid lighter, while viscosity and thermal diffusion resist motion. Instead of drawing prescribed rolls, this experiment integrates three coupled modes and reconstructs velocity and temperature from them.
Why it mattersConnect heat transport, linear instability and deterministic chaos, with trajectories checked against the same equations, steady states and flux diagnostics.
Start with the essentials
The selected horizontal wave number minimizes onset for stress-free isothermal boundaries. Rigid walls have a different threshold.
Circulation, hot–cold contrast and distortion of the mean temperature profile evolve together. RK4 uses a fixed model-time step; the companion starts with a minute circulation offset.
A streamfunction enforces zero divergence and no penetration at both plates. Horizontal boundaries are periodic. Spanwise extrusion adds no third-dimensional dynamics.
Both plate temperatures are fixed. Only the display palette saturates outside the plate range; the reduced model can overshoot, especially under strong drive.
The plate gradient and volume-averaged total heat flux differ during transient storage. On a steady branch they agree; neither is an empirical curve pasted onto the animation.
The nonzero branches exist above onset. The displayed clock is dimensionless model time, not physical seconds. Strong-drive Lorenz dynamics are not quantitative predictions of laboratory turbulence.
Typical misconceptionEvery heated layer shares one universal onset value.
Better mental modelThis model has stress-free isothermal interfaces and a fixed periodic wave number. Its onset must not be confused with rigid no-slip walls.
Typical misconceptionThe two-wing modal trajectory depicts two physical vortices.
Better mental modelThe portrait records amplitudes describing the entire field. Tracers in the apparatus record spatial positions. They share a dynamic state, not a coordinate space.
Typical misconceptionPast the branch instability, the image resolves three-dimensional turbulent flow.
Better mental modelThree modes omit the smaller spatial scales of strongly driven convection. Chaotic reversals belong to the truncated system, not a quantitative turbulent heat-transfer law.
Choose Perturbation decays and advance several model-time units.
What to observe: Circulation fades, mean temperature approaches the linear profile, and both fluxes approach one.Choose Steady rolls and compare early and late heat-flux history.
What to observe: The two fluxes differ during the transient; they converge toward the dashed steady benchmark as the modal orbit settles.Choose Lorenz reversals and keep playing, or increase playback rate.
What to observe: Circulation changes sign and the trajectory circles both branches. A minute initial offset can amplify; playback rate never modifies the equations.Choose No seed and advance, then set a nonzero initial perturbation.
What to observe: The exact zero state does not spontaneously circulate. Setting a seed restarts the experiment from time zero.