“…In the past, these models have been used to simulate the dynamics of discharge at the outlet of intermittent streams (Azarnivand et al, 2020a(Azarnivand et al, , 2020bCamporese et al, 2019;Gutiérrez-Jurado et al, 2019). Moreover, ISSHMs have been used to reproduce the effect of surfacesubsurface interactions on the hydrological response of rivers, not only in terms of surface saturation and groundwater storage patterns but also in terms of flowing stream network dynamics (Ala-Aho et al, 2017;Camporese et al, 2014;Furnari et al, 2024;Gutiérrez-Jurado et al, 2021;Özgen-Xian et al, 2023;Weill et al, 2013;). Nevertheless, the potential of ISSHMs to analyse the processes that drive stream intermittency, for example, by quantifying and analysing the elements of the local water balance that define the surface flow emergence, remains relatively underexploited.…”