“…Although this metric has been widely used to effectively capture spatial differences in riparian vegetation and aquatic macroinvertebrates (Bruno et al., 2014 ; Sánchez‐Montoya et al., 2007 ), other metrics, such as the maximum duration of the dry period or the frequency of drying events, can also be relevant (Arias‐Real et al., 2021 ; Crabot et al., 2020 ; Pineda‐Morante et al., 2022 ; Sánchez‐Montoya et al., 2018 ). The use of in situ hydrological measurements (e.g., data loggers) can better capture recent (e.g., duration of the last dry period) and annual (e.g., annual drying duration and frequency) variability (Arias‐Real et al., 2021 ; Pineda‐Morante et al., 2022 ), but long‐term metrics that represent average conditions in the last decades, such as the mean number of dry days per year and proportion of years with no flow, are particularly relevant and indicated when sampling sites have been surveyed across several years (Bruno, Gutiérrez‐Cánovas, Velasco, et al., 2016a ; Bruno, Gutiérrez‐Cánovas, Sánchez‐Fernández, et al., 2016b ; Belmar et al., 2019 ; Stubbington et al., 2022 ). Finally, that biodiversity surveys were conducted at the end of the wet phase might also have masked flow intermittence effects on biological groups.…”