The Lorenz equations are a set of three differential equations that describe the behavior of a simplified model of convection rolls in the atmosphere, highlighting the concepts of chaos and sensitivity to initial conditions. Introduced by Edward Lorenz in 1963, these equations illustrate how small changes in initial conditions can lead to vastly different outcomes, which is a cornerstone of chaos theory. The Lorenz equations are essential for understanding how chaotic systems can emerge from deterministic rules.
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