“…We note that SES are low-frequency variations of the electric field of the Earth that precede EQs, see, e.g., References [4,[66][67][68][69][70][71][72][73][74][75]. Moreover, characteristic (local) minima of β W have been identified in California [76], Japan [11], Mexico [77][78][79], Eastern Mediterranean [80,81], and Global seismicity [13,82] before the strongest EQs, i.e., those in the EQ catalog having a magnitude M greater than or equal to a target threshold M t , M ≥ M t , and these minima are statistically significant precursors [83,84]. Interestingly, the appearance of these minima has been related [85] to the emission of SES activities and are also simultaneous with changes in the long-range correlations of the EQ magnitude time series [64,86,87] (cf.…”