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Scale parameter
Scale parameter
from Wikipedia

In probability theory and statistics, a scale parameter is a special kind of numerical parameter of a parametric family of probability distributions. The larger the scale parameter, the more spread out the distribution.

Definition

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If a family of probability distributions is such that there is a parameter s (and other parameters θ) for which the cumulative distribution function satisfies

then s is called a scale parameter, since its value determines the "scale" or statistical dispersion of the probability distribution. If s is large, then the distribution will be more spread out; if s is small then it will be more concentrated.

Animation showing the effects of a scale parameter on a probability distribution supported on the positive real line.
Effect of a scale parameter over a mixture of two normal probability distributions

If the probability density exists for all values of the complete parameter set, then the density (as a function of the scale parameter only) satisfies where f is the density of a standardized version of the density, i.e. .

An estimator of a scale parameter is called an estimator of scale.

Families with Location Parameters

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In the case where a parametrized family has a location parameter, a slightly different definition is often used as follows. If we denote the location parameter by , and the scale parameter by , then we require that where is the CDF for the parametrized family.[1] This modification is necessary in order for the standard deviation of a non-central Gaussian to be a scale parameter, since otherwise the mean would change when we rescale . However, this alternative definition is not consistently used.[2]

Simple manipulations

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We can write in terms of , as follows:

Because f is a probability density function, it integrates to unity:

By the substitution rule of integral calculus, we then have

So is also properly normalized.

Rate parameter

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Some families of distributions use a rate parameter (or inverse scale parameter), which is simply the reciprocal of the scale parameter. So for example the exponential distribution with scale parameter β and probability density could equivalently be written with rate parameter λ as

Examples

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  • The uniform distribution can be parameterized with a location parameter of and a scale parameter .
  • The normal distribution has two parameters: a location parameter and a scale parameter . In practice the normal distribution is often parameterized in terms of the squared scale , which corresponds to the variance of the distribution.
  • The gamma distribution is usually parameterized in terms of a scale parameter or its inverse.
  • Special cases of distributions where the scale parameter equals unity may be called "standard" under certain conditions. For example, if the location parameter equals zero and the scale parameter equals one, the normal distribution is known as the standard normal distribution, and the Cauchy distribution as the standard Cauchy distribution.

Estimation

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A statistic can be used to estimate a scale parameter so long as it:

  • Is location-invariant,
  • Scales linearly with the scale parameter, and
  • Converges as the sample size grows.

Various measures of statistical dispersion satisfy these. In order to make the statistic a consistent estimator for the scale parameter, one must in general multiply the statistic by a constant scale factor. This scale factor is defined as the theoretical value of the value obtained by dividing the required scale parameter by the asymptotic value of the statistic. Note that the scale factor depends on the distribution in question.

For instance, in order to use the median absolute deviation (MAD) to estimate the standard deviation of the normal distribution, one must multiply it by the factor where Φ−1 is the quantile function (inverse of the cumulative distribution function) for the standard normal distribution. (See MAD for details.) That is, the MAD is not a consistent estimator for the standard deviation of a normal distribution, but 1.4826... × MAD is a consistent estimator. Similarly, the average absolute deviation needs to be multiplied by approximately 1.2533 to be a consistent estimator for standard deviation. Different factors would be required to estimate the standard deviation if the population did not follow a normal distribution.

See also

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References

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General references

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
In statistics and , a scale parameter is a of a that controls the dispersion or spread of the distribution by stretching or compressing it relative to a standard form with scale equal to 1. Values greater than 1 widen the distribution, increasing variability, while values less than 1 narrow it, reducing variability. Mathematically, a scale family of distributions has probability density functions (pdfs) of the form f(xσ)=1σψ(xσ)f(x \mid \sigma) = \frac{1}{\sigma} \psi\left( \frac{x}{\sigma} \right), where σ>0\sigma > 0 is the and ψ\psi is the pdf of the standard distribution (with σ=1\sigma = 1). This transformation ensures that if XX follows the scaled distribution, then X/σX / \sigma follows the standard form. Many distributions extend this to location-scale families by incorporating a μ\mu, yielding pdfs f(xμ,σ)=1σψ(xμσ)f(x \mid \mu, \sigma) = \frac{1}{\sigma} \psi\left( \frac{x - \mu}{\sigma} \right), where μ\mu shifts the distribution and σ\sigma scales it. In such families, if ZZ is standard (location 0, scale 1), then σZ+μ\sigma Z + \mu generates the general form. Prominent examples include the normal distribution N(μ,σ2)N(\mu, \sigma^2), where the scale parameter σ\sigma equals the standard deviation and directly measures spread around the μ\mu. The gamma distribution features a scale parameter β>0\beta > 0 alongside a α>0\alpha > 0, with αβ\alpha \beta and variance αβ2\alpha \beta^2, making β\beta responsible for horizontal stretching. Similarly, the uses a scale parameter λ>0\lambda > 0 and κ>0\kappa > 0 in its survivor function S(t)=e(λt)κS(t) = e^{-(\lambda t)^\kappa}, influencing the distribution's tail behavior and reliability modeling. The also employs a scale parameter a>0a > 0 with a m>0m > 0, defining heavy-tailed behaviors in economics and finance. Scale parameters are essential in , as they facilitate , hypothesis testing, and model fitting by adjusting for observed data variability. In exponential families and generalized linear models, they often relate to variance functions, enabling robust analysis of or heteroscedasticity. Their role extends to and methods, where scaling generates diverse samples from baseline distributions.

Definition and Mathematical Formulation

Core Definition

In and , a scale parameter is a positive θ > 0 that governs the dispersion or spread of a , effectively stretching or compressing the distribution along the horizontal axis while preserving its overall shape. For a XX with fX(x;θ)f_X(x; \theta), the scaled Y=θXY = \theta X has the transformed density function given by fY(y)=1θfX(yθ),f_Y(y) = \frac{1}{\theta} f_X\left(\frac{y}{\theta}\right), where the factor 1/θ1/\theta ensures the density integrates to 1, maintaining the probabilistic normalization. This transformation highlights how the scale parameter adjusts the variability: larger values of θ widen the distribution, increasing moments like the variance, while smaller values contract it. The scale parameter is distinct from other types of parameters in distribution families. A location parameter μ shifts the entire distribution horizontally without altering its shape or spread, such as translating the support from one interval to another. In contrast, a shape parameter modifies the fundamental form or asymmetry of the density, potentially changing skewness or the presence of tails, but does not simply rescale. Scale parameters thus provide a multiplicative adjustment to the variable's magnitude, independent of these shifts or form changes. Many standard probability distributions are initially formulated in a normalized form with θ = 1, where the spread is fixed (often to unit variance or a specific range), and then generalized by incorporating a to model varying levels of dispersion in real-world data. This approach facilitates theoretical and by separating the effects of scaling from location or shape. To illustrate intuitively, consider the uniform distribution on the interval (0, θ), assuming basic familiarity with probability density functions. Here, θ acts as the , directly setting the length of the interval and thus controlling the variability: the density is constant at 1/θ over (0, θ), so larger θ spreads the probability mass over a wider range, increasing the variance from 0 (degenerate case) to θ²/12. This example demonstrates how scaling intuitively adjusts the "width" of the distribution without shifting its position or changing its flat shape.

Properties of Scale Parameters

Scale parameters exhibit invariance under affine transformations of the , specifically remaining scales when the variable is multiplied by a positive constant. This property ensures that the standardized form of the distribution—obtained by dividing the variable by the scale parameter—is unchanged under such scalings, preserving the of the . The effect of a scale parameter on the moments of a distribution is multiplicative according to the power of the moment. For a XX with standard moments E[Xk]=μkE[X^k] = \mu_k, the scaled variable Y=θXY = \theta X has moments E[Yk]=θkμkE[Y^k] = \theta^k \mu_k, where θ>0\theta > 0 is the scale parameter. In particular, the variance scales quadratically, as \Var(Y)=θ2\Var(X)\Var(Y) = \theta^2 \Var(X). More generally, for a distribution with scale parameter θ\theta relative to a standard form ZZ, the variance satisfies \Var(X)=θ2\Var(Z)\Var(X) = \theta^2 \Var(Z), highlighting how the scale controls the spread without altering higher-order characteristics. Scale parameters are unique in their parameterization due to their and requirement to be positive real numbers, ensuring a one-to-one correspondence with the dispersion of the distribution within the parametric family. This positivity constraint avoids singularities in the function and facilitates , often leading to reparameterizations for interpretability, such as using the standard deviation σ\sigma as the scale parameter in the normal distribution, where the is 1σ2πexp((xμ)22σ2)\frac{1}{\sigma \sqrt{2\pi}} \exp\left(-\frac{(x - \mu)^2}{2\sigma^2}\right)
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