Normal distribution
The normal distribution, also known as the Gaussian distribution, is a continuous probability distribution for a real-valued random variable that is symmetric and bell-shaped, with values most concentrated around its mean and decreasing smoothly away from it.[1] It is defined by two parameters: the mean μ, which specifies the center of the distribution, and the standard deviation σ, which measures the spread or width.[1] The probability density function for a normal random variable X is given byf(x) = \frac{1}{\sigma \sqrt{2\pi}} \exp\left( -\frac{(x - \mu)^2}{2\sigma^2} \right),
where the total area under the curve equals 1, representing the total probability.[1] The normal distribution is the most widely used probability distribution in statistics because it approximates many natural phenomena so well, such as heights, test scores, and measurement errors, due to the influence of numerous small, independent random factors.[2] This ubiquity is largely explained by the central limit theorem, which states that the sampling distribution of the sample mean from any population with finite mean and variance approaches a normal distribution as the sample size increases, regardless of the underlying population distribution. First introduced by Abraham de Moivre in 1733 as an approximation for binomial probabilities and later formalized by Carl Friedrich Gauss in 1809 in the context of astronomical error analysis, the normal distribution underpins much of statistical inference, including hypothesis testing, confidence intervals, and regression analysis.[3]