Abstract:Abstract. Modeling of extremes dry spells in Northern Tunisia, in order to
detect the severity of the phenomenon, is carried out. Dry events are
considered as a sequence of dry days (below a threshold) separated by
rainfall events from each other. The maximum dry event duration follows the
Generalized Extreme Value distribution. The data series adherence to the
probability distribution was verified by the Anderson-Darling test. The
positive trend and non-stationarity of dry spells was verified respectively
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