The Lorenz system — where it appears
Named by 3 essays across one field — each of them below, with the objects they name alongside it.
Three numbers left of a fluid
Saltzman truncated convection to three Fourier modes and Lorenz studied what was left. The result changed science, and it stopped being a description of a fluid at about a fifth of the way to the parameter everybody quotes it at.
A millionth is enough
Two trajectories a millionth apart separate by a factor of e every three-quarters of a second, so a millionfold improvement in the measurement buys about ten seconds of extra prediction. That exchange rate, and not the size of the error, is what limits forecasting.
The truncation that cannot carry three times the heat
Lorenz's three modes give a convecting layer's heat flux in one line — one plus twice (r − 1) over r — and it can never reach three times what conduction carries. The same rolls computed with forty-two modes agree with that line exactly at onset, carry 7.1 per cent more heat at twice the critical Rayleigh number, and twice as much at thirty times it. The ceiling is not in the convection; it is in having one sine to draw the temperature with.
Named alongside it
The objects these essays reach for when they reach for this one.
TruncationConvectionDynamical systemModel limitRayleigh–Bénard convectionBifurcationBoundary layerConvergenceFixed pointForecastingHeat transferThe Lyapunov exponent