The document discusses concepts related to statistical analysis of hydrological data, including measures of skewness, kurtosis, outliers, and the common characteristics of water resources data. Skewness measures asymmetry in a distribution, while kurtosis measures peakedness. Outliers are identified using methods like Chauvenet's criterion, Grubbs' test, and Dixon's Q test. Water resources data commonly has a lower bound of zero, outliers, non-normal distributions, positive skewness, seasonal patterns, and positive autocorrelation between consecutive observations.