For observed data and latent variables , let be the complete-data log-likelihood. From a current parameter , the expectation-maximization algorithm computesand then chooses maximizing this function in its first argument. Thus the E-step averages the missing information conditional on the current model and observed data; the M-step treats those expectations as fixed while maximizing.
For a short proof of likelihood function monotonicity, let . ThenThe Jensen inequality for the logarithm gives . The M-step makes the right side nonnegative. Thus observed likelihood function cannot decrease. This proves the usual EM likelihood monotonicity, while allowing convergence to local stationary points rather than guaranteeing a global maximum.
Put , , and introduce a categorical class label for each observation, encoded by with . Its prior class probability is , and conditional on class the observation probability density function is . Thus its joint observation-label probability density function isIndependence across observations yields the finite Gaussian mixture with a common variance complete-data likelihood functionSumming over the two possible labels at each observation recovers , the observed-data likelihood function. The product requested in the PDF is therefore a joint complete-data likelihood function. Strictly conditioning on would remove the factors ; the PDF's conditional notation for this joint product is imprecise.
The E-step uses the posterior class probabilitiesLet , so . Up to constants, the expected complete-data log-likelihood isMaximizing the first term with gives . Differentiating in each gives . After these updates, maximizing in the shared variance givesThe residuals use the new component means, while the weights remain from the old parameters. The divisor is , not , because this is a maximum-likelihood update. Starting with and gives positive responsibilities and positive ; a zero effective component size at a boundary would leave its mean unidentified. These are the EM for Gaussian mixtures with a common variance transitions.
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