“…It is essential to implement studies with a long-term duration and a wide spatial perspective. In fact, in order to perform appropriate monitoring of water resources and in particular to intercept potential drought events in advance, it is necessary, on one hand, according to the traditional methodological approach, to determine the frequency, duration, and spatial domain over which the phenomena extend [44]; on the other hand, it must be considered that the climate processes tend to propagate through the hydrological cycle [22,24], gradually influencing the different components (i.e., precipitation, soil moisture, infiltration, groundwater recharge, and spring flows). In this regard, several authors ( [23,45] among others) argue that the propagation of the drought signal reaches the groundwater components often slowly or not at all, but when this occurs, drought produces severe and long-lasting consequences.…”