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#AlgorithmsFromAtoZ E: Error Diffusion (Floyd–Steinberg dithering)

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The π in the normal distribution has a geometric origin. It comes from a famous mathematical result known as the Gaussian integral. ∫₋∞^∞ e^(−x²) dx = √π The interesting part is that e^(−x²) has no elementary antiderivative. Yet its integral over the entire real line can be calculated exactly. The solution involves turning a one-dimensional integration problem into a two-dimensional one. The resulting function, e^(−(x²+y²)), has circular symmetry, and polar coordinates reveal where π enters the calculation. This result is fundamental to probability theory. The familiar factor 1/(σ√(2π)) in the normal distribution comes from the same integral. It ensures that the total probability across all possible values is exactly 1. But its applications extend well beyond statistics. In engineering, Gaussian distributions are commonly used to model measurement errors and noise. With independent, zero-mean Gaussian errors of equal variance in an additive-error model, maximum-likelihood estimation is equivalent to minimizing the sum of squared residuals. Gaussian functions also appear in heat diffusion, where they describe how an initially concentrated point source spreads through an unbounded, homogeneous medium. In Fourier analysis, the transform of a Gaussian is another Gaussian, up to scaling. This property is useful in signal processing and image filtering. The same mathematical function connects probability distributions, statistical estimation, heat transfer, and frequency analysis. And the √π in its integral ultimately comes from the geometry of the plane.

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