The aquatic sciences have a long tradition of connecting hydrologic variability to ecosystem function by characterizing ecologically important components of the flow regime, such as the timing, duration, frequency, magnitude, and rate of change of flow (Poff et al., 1997). While the flow regime paradigm continues to be important for advancing the understanding and management of lotic ecosystems (Palmer & Ruhi, 2019), there is a need to extend this perspective to aquatic systems that dry, referred to as non-perennial rivers (Busch et al., 2020). Non-perennial rivers comprise the majority of global river networks (Datry, Larned, & Tockner, 2014;Goodrich et al., 2018;Yu et al., 2020) and are predicted to increase in extent due to further human alterations and climate change (Jaeger et al., 2014;Ward et al., 2020). From local to global scales, non-perennial rivers play an important role in material storage and downstream transport (Jaeger et al., 2017), habitat partitioning for riparian plants and aquatic organisms (Schilling et al., 2020), and biogeochemical processing of carbon (Shumilova et al., 2019;von Schiller et al., 2019).