“…For a fixed mean precipitation, the growing scale parameter implies increasing of the percentile for a relatively large (more than 10 mm/day) precipitation value. Quantitative estimation of the shape and scale parameters was performed using maximum likelihood method of Greenwood and Durand (1960), based on ln(hxi)Àhln(x)i, hi being the averaging operator, which is more effective than the traditional moment estimators (Wilks, 1990(Wilks, , 1995 and more accurate for the data used than the Thom (1958) method. From the Gamma distribution, we have derived the other statistical characteristics of daily precipitation, such as different percentiles and others.…”